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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar crusts on some steep  SE to West  slopes at TL. Extensive wind effect in the alpine, less at treeline. In thick snowpack areas, the Dec 10th weak layer of facets is now down 100-150cm with a stronger snowpack below. In thin snowpack areas, there is little separation between Dec 10 and the weak depth hoar/ facets sitting 40 cm above the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">Warm temps and solar input moistening steep south facing slopes. 5-10mm surface hoar is present in sheltered areas. Wind effect is visible in exposed areas from previous moderate-strong SW winds. A generally strong mid snowpack overlies deep persistent weakness. Use caution in shallow areas where these deep weakness might be more reactive. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A temperature inversion has promoted slab formation at tree-line and alpine elevations, as well as helped create a surface crust, especially on steep solar aspects. Isolated wind slabs exist in the alpine in exposed areas and near ridge lines on all aspects. The Jan 2 freezing rain crust is down ~90cm. The Nov 21st interface is now 1-2m in deep.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar crusts on some steep SE to West slopes at TL. Extensive wind effect in the alpine, less at treeline. In thick snowpack areas, the Dec 10th weak layer of facets is now down 100-150cm with a stronger snowpack below. In thin snowpack areas, there is little separation between Dec 10 and the weak depth hoar/ facets sitting 40 cm above the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar crusts on some steep SE to West slopes at TL. Surface hoar development at treeline.  In thick snowpack areas, the Dec 10th weak layer of facets is now down 100-150cm with a stronger snowpack below. In thin snowpack areas, there is little separation between Dec 10 and the weak depth hoar/ facets sitting 40 cm above the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">Surface conditions vary thanks to the past weeks drought - a thin crust on steep solar aspects, 5-10mm surface hoar in sheltered areas, and wind effect in exposed areas from moderate-strong SW winds. A generally strong mid snowpack overlies deep persistent weaknesses. Use caution in shallow areas where these deep weakness might be more reactive. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A temperature inversion has promoted snow settlement at tree-line and alpine elevations. A crust has developed on steep solar aspects, while surface hoar has been observed up to 20mm in sheltered areas. The Jan 2 freezing rain crust is down ~90cm while the Nov 21 interface is down ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar crusts on some steep SE to West slopes at TL. Surface hoar development at treeline. In thick snowpack areas, the Dec 10th weak layer of facets is now down 100-150cm with a stronger snowpack below. In thin snowpack areas, there is little separation between Dec 10 and the weak depth hoar/ facets sitting 40 cm above the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar crusts on some steep SE to West slopes at TL. Surface hoar development at treeline. In thick snowpack areas, the Dec 10th weak layer of facets is now down 100-150cm with a stronger snowpack below. In thin snowpack areas, there is little separation between Dec 10 and the weak depth hoar/ facets sitting 40 cm above the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">Surface conditions vary from a thin crust on steep solar aspects, 5-10mm surface hoar in sheltered areas, good powder skiing in sheltered locations, and wind effect in exposed areas from recent moderate-strong SW winds. A generally strong mid snowpack overlies the deep persistent weaknesses of facets and depth-hoar.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A temperature inversion has promoted snow settlement at treeline and alpine elevations. Hard wind slabs are present in alpine areas exposed to downflow winds. A crust has developed on steep solar aspects, while surface hoar has been observed up to 20mm in sheltered areas. The Nov 21 persistent weak layer is down ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm off storm snow on Thursday has fallen over a variety of hard bed surfaces including newly buried Surface Hoar 1600-1900m and a supportive temperature crust up to 2000m. A strong Midpack sits on top of a faceted base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar crusts on some steep SE to West slopes at TL. Surface hoar development below treeline. It has become increasingly hard to find midpack instabilities in Yoho. Basal instabilities are common - not quite depth hoar, just large facets and rounded facets. Treeline depths range from 150cm to 200cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40 to 60cm of settled snow sits on large facetted grains of varying strength. Treeline snow depths generally range from 100 to 150 cm. The facets in the lower portion of the snowpack are failing in tests often in the moderate range. Alpine, and open treeline areas can have great variability in snow depth and layering due to local winds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">Last weeks surface hoar and suncrust will be buried under the incoming new snow. These layers will be the new focus of concern. The additional load may well awaken the deeply buried basal instabilities and wind slab activity can be expected at treeline and above. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of new snow fell overnight with light southerly winds. The new snow conceals hard wind slabs in exposed alpine areas, a crust on steep solar aspects, and large surface hoar in sheltered areas. The Nov 21 persistent weak layer is down ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Basal instabilities are common in Yoho. Large facets and rounded facets are overlain by 100 to 150cm of settled snow.  Treeline depths range from 150cm to 200cm. Thinner snowpack areas in the 75-100cm range are thought to be less stable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40 to 60cm of settled snow sits on large facetted grains of varying strength. Treeline snow depths generally range from 100 to 150 cm. The facets in the lower portion of the snowpack are failing in tests often in the moderate range. Alpine, and open treeline areas can have great variability in snow depth and layering due to local winds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">New wind slab, especially around the Icefields can be expected at ridge tops and immediate lees. They will lie over a mix of old surfaces (facets and/or surface hoar) and may show some inconsistent reactivity, treat with caution. All this, over a generally strong mid-pack over the deep persistent weaknesses of facets and depth-hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm of storm snow in the last 48hrs with light to moderate South wind. Storm snow will hide underlying wind slab in the alpine, a crust on steep solar aspects, and large surface hoar in sheltered areas. The Nov 21 persistent weak layer is down ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Basal instabilities are common in Yoho. Large facets and rounded facets are overlain by 100 to 150cm of settled snow. Treeline depths range from 150cm to 200cm. Thinner snowpack areas in the 75-100cm range are thought to be less stable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 to 15 cm of recent snow buried suncrusts and some surface hoar. Moderate to Strong SW winds created small soft winslabs in the alpine Friday and Saturday. Of greatest concern are the weak facets and depth hoar in the lower half of the snowpack. In thin snowpack areas (150cm or less) triggering a slab over this layer is more likely. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">New wind slab in the alpine can be expected at ridge tops and immediate lees. 10cm of new, low density snow lies over a mix of old surfaces (facets and/or surface hoar). This, over a generally strong mid-pack sitting on the deep persistent weaknesses of facets and depth-hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm of storm snow in the last 48hrs mod South wind yesterday. Limited storm slab development observed on field trips yesterday but our obs limited to TL and below. Storm snow will hide underlying wind slab in the alpine, a crust on steep solar aspects, and large surface hoar in sheltered areas. The Nov 21 persistent weak layer is down ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 to 15 cm of recent snow buried suncrusts and some surface hoar. Moderate to Strong SW winds created small soft winslabs in the alpine Friday and Saturday. Of greatest concern are the weak facets and depth hoar in the lower half of the snowpack. In thin snowpack areas (150cm or less) triggering a slab over this layer is more likely. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15 cm of snow sits over the Jan 17 layer of surface hoar, or sun crust. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">New wind slab in the alpine can be expected at ridge tops and immediate lees. 10cm of new, low density snow overlies a mix of old surfaces (facets and/or surface hoar and sun crust). This, over a generally strong mid-pack sitting on the deep persistent weaknesses of facets and depth-hoar.  Thin sun crust on steep due south.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm of storm snow overlies a wide variety of surfaces depending on aspect, elevation, and drainage; including but not limited to surface hoar in sheltered locations to unreactive wind slabs in the alpine. The new snow was accompanied by extreme winds on Saturday, forming slabs in specific areas throughout the park. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm of recently wind affected snow is sitting on either a suncrust below 2000m on solar aspects or spotty surface hoar in sheltered areas between 1600 and 1900m. This may be a problem layer as we see more snow this week. The midpack is strong in deep snowpack areas, but the facets lingering at the bottom remain a concern in thinner areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15 cm of snow sits over the Jan 17 layer of surface hoar, or sun crust. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas (i.e. less than 150 cm deep) triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15 cm of snow sits over the Jan 17 layer of surface hoar, or sun crust. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">New wind slab in the alpine can be expected at ridge tops and immediate lees. 10cm of new, low density snow overlies a mix of old surfaces (facets and/or surface hoar and sun crust). This, over a generally strong mid-pack sitting on the deep persistent weaknesses of facets and depth-hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is settled and strong except for a few layers of note. First and foremost, the Jan17th SH layer buried 15-30cm. This layer is only problematic where the wind has created soft slabs above it. The buried PWLs (Nov 21st and Oct Crust) have been unreactive in stability tests, but may wake up later in the season, or in shallow areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15 cm of snow sits over the Jan 17 layer of surface hoar, or sun crust. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last few days. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">New wind slabs and wind effect in the alpine and exposed TL. 10cm of new, low density snow overlies a mix of old surfaces (facets and/or surface hoar and sun crust). This, over a strong mid-pack sitting on the deep persistent weaknesses of facets and depth-hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">6cm of new snow rests on a strong, settled snowpack with only a few layers of note. The Jan17th SH layer buried 15-30cm and seems most problematic where the wind has created soft slabs above it. The buried PWLs (Nov 21st and Oct Crust) have been unreactive in stability tests, but may wake up later in the season, or in shallow areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of recently wind affected snow has gradually loaded either a suncrust below 2000m on solar aspects or spotty surface hoar in sheltered areas between 1600 and 1900m. This may be a problem layer when we see more snow. The midpack is strong in deep snowpack areas, but the facets lingering at the bottom remain a concern in thinner areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of snow sits over previous surfaces.  Thin wind slabs can be found in alpine lee areas from previous strong winds. Of greatest concern are the weak facets and depth hoar at the base of the snowpack.  In Little Yoho these are not as prevalent as E of the divide due to deeper snow depths, but are still well developed in thin snowpack areas.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last few days. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">New wind slabs, variable levels of misery, er...wind effect and sastrugi in the alpine and exposed TL areas. In sheltered areas, 10cm of low density snow overlies a mix of old surfaces (facets and/or surface hoar and sun crust). This, over a strong mid-pack sitting on the deep persistent weaknesses of facets and depth-hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm in the past 48hrs rests on a strong, settled snowpack with only a few layers of note. The Jan17th surface hoar (20mm) is buried 20-40cm and seems most problematic at 1600-2100m in sheltered areas. The buried PWLs (Nov 21st and Oct Crust) have been unreactive in stability tests, but could be trigger from steep, shallow, rocky areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of recently wind affected snow sits atop a crust layer below 2000m . The midpack is strong in deep snowpack areas, but the facets lingering at the bottom remain a concern in thinner areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30cm of generally low density snow sits over previous surfaces. In deeper snowpack areas in Little Yoho the main concern is for new snow instabilities. Profiles are showing no results in the deeper layers previously found active (Dec 10). In thin areas, basal facets are well formed and still a concern for triggering larger avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last week over isolated suncrusts and surface hoar. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">Warming in the region Saturday will create isolated moist surface snow, snowballing, and likely wet loose slides. Wind effect well pronounced in the alpine and exposed TL areas. 10cm of low density snow overlies a mix of old facets and/or surface hoar and sun crust. A strong mid-pack sits over a deep persistent weaknesses of facets and depth-hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Most open terrain in the alpine has been wind affected. In specific locations, strong S winds have redistributed storm snow and created loaded pockets and wind slabs on lee and cross-loaded features at treeline and above. The Jan 17 persistent weak layer down 30cm is surface hoar in sheltered areas and sun crust on solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last week over isolated suncrusts and surface hoar. Thin wind slabs can be found in alpine lee areas from strong SW winds on Saturday. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last week over isolated suncrusts and surface hoar. Widespread wind effect in the alpine creeping into treeline with current winds. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warming in the region has created isolated moist surface snow conditions up to 2200m. Wind effect is well pronounced in the alpine and exposed TL areas. 10cm of low density snow overlies a mix of old facets and/or surface hoar and sun crust. A strong mid-pack sits over a deep persistent weaknesses of facets and depth-hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In specific locations, strong S winds have redistributed storm snow and created loaded pockets and wind slabs on lee and cross-loaded features at treeline and above. The Jan 17 persistent weak layer down 30cm is surface hoar in sheltered areas and sun crust on solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of recently wind affected snow sits atop a crust layer below 2000m . The midpack is strong in deep snowpack areas, but the facets lingering at the bottom remain a concern in thinner areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last week over isolated suncrusts and surface hoar. Widespread wind effect in the alpine creeping into treeline with current winds. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last week over isolated suncrusts and surface hoar. Widespread wind effect in the alpine. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm new snow fell on Sunday with NW winds, over hard surfaces in wind exposed Alpine terrain, and on steep solar aspects.  A layer of weak surface hoar is now buried 15-20cm deep. Below, a strong mid-pack sits over weak, large facets and depth-hoar in the lower third of the snowpack (giving sudden results in snowpack testing Saturday).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In specific locations, strong to extreme S winds have redistributed storm snow and created loaded pockets and wind slabs on lee and cross-loaded features at treeline and above. The Jan 17 persistent weak layer down 30cm is surface hoar in sheltered areas and sun crust on solar aspects. The overlying 30cm has settled into a cohesive soft slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow over the last week over isolated suncrusts and surface hoar. Widespread wind effect from previous extreme winds. Of greatest concern are the weak facets and depth hoar at the base of the snowpack which only exist in thin areas of Little Yoho ( under 150cm). Otherwise the facets are of little concern. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow sits on top of isolated sun-crusts and surface hoar. Possible new soft wind slabs in lee alpine areas. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snowfall on Sunday with SW - NW winds created wind slabs in lee and cross-loaded terrain. Surfaces became moist on solar slopes at treeline Monday. A layer of weak surface hoar is now buried 10-20cm deep. Below, a strong mid-pack sits over depth-hoar in the lower third of the snowpack (giving sudden results in snowpack testing Saturday).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong southerly winds have created a variable wind slab in lee and cross-loaded alpine and tree-line features. The Jan 17 persistent weak layer (surface hoar or suncrust) is buried 30-50cm, and is most reactive in sheltered areas below tree-line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20cm of snow from Monday's upslope storm sits on a variable, wind affected bed surface . A Sun crust is forming on solar aspects. The midpack is strong in deep snowpack areas, but the facets lingering at the bottom remain a concern in thinner areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow sits on top of isolated sun-crusts and surface hoar. Possible new soft wind slabs in lee alpine areas. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. In thinner snowpack areas with less than 150 cm of snow, triggering a slab on these facets is more likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow sits on top of isolated sun-crusts and surface hoar. Possible soft wind slabs in lee alpine areas. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. Triggering a slab is more likely in thin snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snowfall on Sunday with SW - NW winds created wind slabs in lee and cross-loaded terrain. Surfaces became moist on solar slopes at treeline Monday. A layer of weak surface hoar is now buried 10-15cm deep. Below, a strong mid-pack sits over depth-hoar in the lower third of the snowpack (giving sudden results in snowpack testing Saturday).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extreme winds over the weekend created wind slabs on specific terrain features in the alpine and treeline. Soft slabs exist at treeline and below as the January 17th surface hoar is being incrementally buried. This layer is now buried 25-45cm, it is most reactive between 1400-1900m, and where it overlies a crust on steep solar aspects.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow sits on top of isolated sun-crusts and surface hoar. Possible soft wind slabs in lee alpine areas. Of greatest concern are the weak facets and depth hoar at the base of the snowpack. Triggering a slab is more likely in thin snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A 40cm to 100cm bridge or slab overlies 20 to 50 cm of large facets and depth hoar. Many open areas have been affected by the wind. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunday's snowfall along with SW - NW winds created wind slabs in lee and cross-loaded terrain. Expect a crust on solar slopes at treeline. The upper snow pack continues to settle and the layer of weak surface hoar is now buried 5-10cm deep. Below, a strong mid-pack sits over depth-hoar in the lower third of the snowpack giving sudden results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extreme winds over the weekend created wind slabs on specific terrain features in the alpine and treeline. Soft slabs exist at treeline and below as the January 17th surface hoar has been incrementally buried. This layer is now buried 25-45cm, it is most reactive between 1400-1900m, and where it overlies a crust on steep solar aspects.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Most regularly skied areas of Yoho have a deep snowpack that can bridge underlying problems. Isolated, shallow snowpack areas may still be triggered. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect in alpine from last weeks strong winds. The mid-pack is increasingly settled (up to P) down to the Dec 10 interface (down 60-130 cm). In shallower snowpack areas weak facets exist below the Dec 10 interface, and stability tests show moderate-hard results within the facets.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasted storm snow over this weekend (potentially up to 50cm), will change everything in the snowpack. The existing upper snow pack continues to settle over surface hoar, down 5-10cm deep. Solar aspects have buried surface sun/temperature crusts at TL and below. Below that, a strong mid-pack sits over a deep persistent weakness. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of new snow overnight with moderate S winds. New snow sits atop hard wind slabs in the alpine and exposed areas at treeline. The January 17 surface hoar is buried 30-50cm and is most reactive between 1400-1900m, and where it overlies a crust on steep solar aspects. A reloaded crust from November has been reactive on steep south aspects.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20cm settled powder has been redistributed by strong to extreme west winds in the alpine and at treeline. This sits on a variety of wind affected surfaces and a melt freeze crust below 2000m. The midpack is strong in deep snowpack areas, but the facets lingering at the bottom remain a concern in thinner areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Some wind effect in alpine and small windslabs exist in immediate lees. The mid and lower pack is generally well settled.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35 cm of new snow with moderate SW-SE winds is building slabs in lee areas of the alpine. The mid-pack is quite dense above the Dec 10 interface down 70-140 cm. In shallower snowpack areas weak facets exist below the Dec 10 interface, with moderate-hard test results in the facets. In deeper snowpack this basal weaknesses is less pronounced</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasted storm snow over this weekend, 18cm at the time of report, (potentially a further 30cm), will change everything. The existing upper snow pack continues to settle over surface hoar, now down 30cm. Solar aspects have buried surface sun/temperature crusts at TL and below. Below that, a strong mid-pack sits over a deep persistent weakness. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">35cm of new snow has fallen in the past 24hrs with moderate south winds. New snow sits atop hard wind slabs in the alpine. The January 17 surface hoar is buried 60cm and is most reactive between 1400-1900m, and where it overlies a crust on steep solar aspects. Several crusts exist in the upper snowpack on steep south aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35 cm of new snow with moderate SW-SE winds is building slabs in lee areas of the alpine. In some treeline locations a thin weak layer is found down 20-30 cm that was reactive to skiers Thursday. The mid and lower snowpack have few weaknesses in most areas, however concern remains for the weak facets below the Dec 10 interface in shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25-40cm of new snow with moderate to strong variable winds. Up to 65cm sits over the Jan.17 surface hoar which has been found up to 2300m. The mid-pack is quite dense above the Dec 10 interface down 80-160 cm. In shallower areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snowpack this basal weaknesses is less pronounced</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40cm new snow throughout the forecast region. This puts the Jan18 buried surface hoar, down 50cm. Previous to this storm a strong midpack was bridging the basal weakness. Storm snow may overload that bridging and, large avalanches could be expected to travel full path if triggered. Avoid all avalanche terrain until the new snow has time to settle.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At 1900m upwards of 75cm of storm snow has fallen in the past 48hrs with mod to strong S'ly winds. New snow sits atop hard wind slabs in the alpine and Jan 31 surface hoar at and below treeline. January 17 surface hoar is buried 70cm and is most reactive between 1400-1900m, and where it overlies a crust on steep solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-40cm of new snow with moderate to strong variable winds are building slabs in lee areas of the alpine. In locations up to 2200m a thin but reactive layer of surface hoar and/or crust is found down 60-70cm. The mid and lower snowpack have few weaknesses, however concern remains for the weak facets below the Dec 10 interface in shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-45cm of recent storm snow is being redistributed into windslabs above treeline. Up to 65cm sits over the Jan.17 surface hoar which has been found up to 2300m. In shallower areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snowpack this basal weaknesses is less pronounced</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50cm new snow in the past 48 hours and recent strong winds. This overlies a variety of surfaces from previous wind effect, sun crust and the Jan 18 surface hoar (most prominent in sheltered locations TL and below). We suspect the recent winds and new snow will be overloading the well settled mid pack and producing large scale avalanches</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At 1900m upwards of 70cm of storm snow in the past 72hrs with mod to strong S'ly wind. Wind is now shifted to NE mod. New snow sits atop hard wind slabs in the alpine and Jan 31 surface hoar at and below treeline. January 17 surface hoar is buried 90cm+ and is most reactive between 1400-1900m, and where it overlies a crust on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-45cm of recent storm snow is being redistributed into windslabs above treeline.&nbsp; In locations up to 2200m a thin but reactive layer of surface hoar (Jan 17) and/or crust is found down 60-70cm. The mid and lower snowpack have few weaknesses, however concern remains for the weak facets below the Dec 10 interface in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent snow and wind have created wind slab on lee alpine slopes. At treeline elevations, up to 65cm of snow sits over the Jan.17 surface hoar. In shallower areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snow packs this basal weaknesses is less pronounced.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">50cm recent storm snow came with strong Northerly winds. This storm snow overloaded the Jan 18 persistent weakness (SH in sheltered areas, crust on exposed solar slopes) in deeper snowpack areas, and the weak and facetted base of the snowpack in shallow areas (deep persistent weakness), resulting in a natural cycle of large avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At treeline we received upwards of 70cm of storm snow over the weekend with strong Sth winds and mild temps. The storm snow is sitting over the Jan 31st crust on solar asp at TL and BTL. In the Alpine, the storm snow overlies old dormant wind slabs. Reverse loading over the past 24 hours will have relocated the storm snow at TL and in the Alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-30cm of recent low density snow has been redistributed by previous strong to extreme west winds, and more recent moderate NE winds in the alpine and at treeline. This sits on a melt freeze crust below 2000m. The midpack is strong in deep snowpack areas, but the facets lingering at the bottom remain a concern in thinner areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent snow and wind have created wind slab on lee alpine slopes. At treeline elevations, up to 65cm of snow sits over the Jan.17 surface hoar. In shallower areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snow packs this basal weaknesses is less pronounced.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wide spread wind effect above treeline has created wind slab on NE to SE aspects. At treeline elevations, up to 65cm of snow sits over the Jan.17 surface hoar. In shallower areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snow packs this basal weakness is less pronounced. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">50cm recent storm snow was followed by strong Northerly winds. This storm snow overloaded the Jan 18 persistent weakness (srfce hoar up to 10mm in sheltered areas at lower elevations, crust on steep solar slopes, and facets on Northerly alpine slopes), and the deep persistent weakness (basal facets - found predominantly in shallow snowpack areas).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">~70cm of storm snow overlies the Jan 17th SH and ~60cm over the Jan 31st layer. Strong winds that came with the storm redistributed the storm snow in the alpine and exposed areas of TL. Wind slabs and buried crusts exist on specific terrain features depending on aspect and elevation. Low-density new snow can be found in sheltered locations.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wide spread wind effect above treeline has created wind slab on NE to SE aspects. At treeline elevations, up to 65cm of snow sits over the Jan.17 surface hoar. In shallower areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snow packs this basal weakness is less pronounced. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wide spread wind effect above treeline has created wind slab on NE to SE aspects. Below treeline,30 to 50cm of snow sits over the Jan.17 surface hoar which causes the odd settlement but little activity so far. In shallow areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snow packs this basal weakness is less pronounced. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">50cm from Feb 2nd was followed by strong Northerly winds. This snow overloaded; the Jan 18 persistent weaknesses such as surface hoar 10mm in sheltered areas at lower elevations, crust on steep solar slopes, and facets on Northerly alpine slopes; and the deep persistent basal facet and depth hoar weakness - particularly in shallow snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temps promoting surface faceting. ~70cm of storm snow overlies the Jan 17th SH and ~60cm over the Jan 31st layer. Strong winds that came in with the storm redistributed the storm snow in the alpine and exposed areas of TL. Wind slabs and buried crusts exist on specific terrain features depending on aspect and elevation. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wide spread wind effect above treeline has created wind slab on NE to SE aspects. Up to 65cm of snow sits over the Jan.17 surface hoar, especially prevalent between 1800-2000m. In shallower areas weak facets and depth hoar exist below the Dec 10 interface. In deeper snow packs this basal weakness is less pronounced. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">50cm from Feb 2nd was followed by strong Northerly winds. This snow overloaded the Jan 18 persistent weaknesses which is surface hoar 10mm in sheltered areas at lower elevations, crust on steep solar slopes, and facets on Northerly alpine slopes. A deep persistent basal facet and depth hoar weakness exists particularly in shallow snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A thin sun crust has formed on steep solar aspects in alpine. Cold temps promoting near surface faceting and softening wind slabs that exist in alpine and exposed areas at tree line. The storm snow has settled has to ~50cm. The Jan 31 and Jan 17 interfaces (surface hoar and sun crust) are down ~50cm and ~70cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-30cm of facetting storm snow has been redistributed by SW winds. This new snow sits on a variety of previous wind affected surfaces including a melt freeze crust up to 2000m on all asp. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The Midpack is strong in deep snowpack areas but the facets at the base of the snowpack remain a concern in shallow areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">50cm from Feb 2nd was followed by strong Northerly winds and cold temperatures. This snow overlies a dormant but persistent weaknesses of surface hoar, crusts, and/or facets. Cold temps have weakened the structure of the slab over this layer and it lays dormant, for now. A deep persistent basal facet/depth hoar weakness exists in shallow areas.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A thin sun crust has formed on steep solar aspects in the alpine. Cold temperatures are promoting near surface faceting and softening wind slabs that exist in alpine and exposed areas at tree line. The storm snow has settled has to ~50cm. The Jan 31 and Jan 17 interfaces (surface hoar and sun crust) are down ~50cm and ~70cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">50cm from Feb 2nd was followed by strong Northerly winds and cold temperatures. This snow overlies a dormant but persistent weaknesses of surface hoar, crusts, and/or facets. Cold temps have weakened the structure of the slab over this layer and it lays dormant, for now. A deep persistent basal facet/depth hoar weakness exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme north winds created wind slabs and loaded pockets on lee features. Wind slabs sit atop a crust on steep solar aspects in the alpine. Cold temperatures are promoting near surface faceting. The storm snow has settled to ~50cm. The Jan 31 and Jan 17 interfaces (surface hoar and sun crust) are down ~50cm and ~70cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">50cm from Feb 2nd was followed by strong N winds and cold temperatures. This snow overlies a dormant but persistent weakness of surface hoar, crusts, and/or facets. Cold temps have weakened the structure of the slab over this layer and it's generally dormant, for now. A basal depth hoar weakness exists especially shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday's Strong N through E winds have created widespread wind slabs, note reverse loading. Wind slabs sit atop a crust on steep solar aspects in the alpine. Cold temps are promoting near surface faceting. The storm snow has settled to ~50cm. The Jan 31 and Jan 17 interfaces (surface hoar and sun crust) are down ~50cm and ~70cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">50cm from Feb 2nd was followed by strong N winds. Ongoing cold temps have weakened the structure of the slab over the persistent weakness below, which consists of surface hoar, crusts, and/or facets. The basal snowpack is structurally weak in shallow areas, consisting primarily of facets/depth hoar (ongoing cold temps are not helping).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Saturday's strong NE winds have created widespread wind slabs. These lay on a suncrust on S and W alpine aspects. Storm snow has been redistributed and is faceting due to the cold temps. Weak layers of concern, the Jan 31 and Jan 17 interfaces (surface hoar and sun crust), are down ~50cm and ~70cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of facetting storm snow has added to the formation of Windlsab in the alpine and at ridge top. Windslab will continue to be a primary concern on Tuesday as the forecasted snow is accompanied by moderate - extreme winds. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The Midpack is strong in deep snowpack areas but the facets at the base of the snowpack remain a concern in shallow areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. Overall the snowpack is strong. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm and is producing moderate, planar shear tests, but there is minimal slab overlying the layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm, producing moderate tests results. The lower snowpack consist of a strong mid-pack sitting over a weak faceted basel structure.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Ongoing cold temps have weakened the structure of the upper snowpack. There is no longer a slab over the persistent weakness sitting down 30-40cm (surface hoar, crusts, and/or facets). The basal snowpack is structurally weak in shallow areas, consisting primarily of facets/depth hoar (cold temps continue to develop this deep persistent weakness).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Saturday's strong NE winds have created widespread wind slabs. These lay on a suncrust on S and W alpine aspects. Storm snow has been redistributed and is faceting due to the cold temps. Weak layers of concern, the Jan 31 and Jan 17 interfaces (surface hoar and sun crust), are down ~50cm and ~70cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine areas are a mix of wind blasted and/or soft (faceted) surface snow depending on location - sheltered areas have 40 cm ski penetration. The Jan 17 surface hoar/crust interface can be found below 2200 m down 40-60 cm, producing moderate tests results. The lower snowpack consist of a strong mid-pack sitting over a weak faceted basel structure.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow overlies low density facets that formed near the surface during the current cold spell. These surface conditions can produce dry loose avalanches in steep places, but slab formation has been minimal. The distribution of the Jan 17 SH is spotty, but in some areas </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1ca81590-cf89-4632-ae86-d5ec3bd845d8" target="_blank"><span class="s_9255B882">(Kootenay) it appears prominent;</span></a><span class="s_AA239A9B"> strength tests are hard &amp; sudden</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Some wind affect noted in the alpine and at tree line. Due to the cold temperatures there seems to be no slab over the persistent weakness sitting down 35-45cm (surface hoar, crusts, and/or facets). The bottom of the snowpack is structurally weak especially in shallow snowpack areas, consisting primarily of facets/depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A dusting of new snow covers old hard slabs, and wind scoured surfaces in the ALP and exposed areas of TL. These hard slabs are from Saturday's wind event; strong N-NE winds reverse loaded any available snow onto solar aspects, over a thin sun crust. The Jan 17th PWL is buried approximately 50-70cm at TL and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-45cm of new storm snow in the past 24h. This new snow sits over a variety of wind affected surfaces including pockets of Windslab near ridgetop. We expect the storm snow to be reactive to human traffic through the weekend. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The Midpack is strong in deep snowpack areas but this increase in loading will stress the weak, facetted basal snowpack. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow overlies low density facets that formed near the surface during the current cold spell. These surface conditions can produce dry loose avalanches in steep places, but slab formation has been minimal. The distribution of the Jan 17 SH is spotty, but in some areas </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1ca81590-cf89-4632-ae86-d5ec3bd845d8" target="_blank"><span class="s_9255B882">(Kootenay) it appears prominent;</span></a><span class="s_AA239A9B"> strength tests are hard &amp; sudden</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow overlies low density facets that formed near the surface during the current cold spell. These surface conditions can produce dry loose avalanches in steep places, but slab formation has been minimal. The distribution of the Jan 17 SH is spotty, but in some areas </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1ca81590-cf89-4632-ae86-d5ec3bd845d8" target="_blank"><span class="s_9255B882">(Kootenay) it appears prominent;</span></a><span class="s_AA239A9B"> strength tests are hard &amp; sudden</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Some wind affect noted in the alpine and at tree line. Due to the recent cold temperatures there seems to be no slab over the persistent weakness sitting down 35-45cm (surface hoar, crusts, and/or facets). The bottom of the snowpack is structurally weak especially in shallow snowpack areas, consisting primarily of facets and depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A dusting of new snow covers old hard wind slabs, and scoured surfaces in the ALP and exposed areas of TL. Cold temperatures continue to promote near surface facetting at all elevations; deteriorating the bonds of the upper snowpack. Wind slabs were most active on solar asp, where crusts are buried. The Jan 17 SH is down 50-70cm at TL and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-45cm of snow in the past 48h with moderate SW winds have created reactive soft slabs. These new storm slabs sit over a variety of wind affected surfaces including pockets of Windslab near ridgetop. The Midpack is strong in deep snowpack areas but this increase in loading will stress the weak, facetted basal snowpack. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow overlies low density facets that formed near the surface during the current cold spell. These surface conditions can produce dry loose avalanches in steep places, but slab formation has been minimal. The distribution of the Jan 17 SH is spotty, but in some areas </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/1ca81590-cf89-4632-ae86-d5ec3bd845d8" target="_blank"><span class="s_9255B882">(Kootenay) it appears prominent;</span></a><span class="s_AA239A9B"> strength tests are hard &amp; sudden</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 40 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of intense solar radiation and most notably, sustained cold temperatures promoting faceting. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Cold temperatures have faceted the upper snowpack, leaving no slab over a weakness down 40cm (surface hoar, facets, and/or crust).&nbsp; However, the stronger mid-pack could act as a slab over weak depth hoar, which comprises the lower third of the snowpack. This is pronounced in shallow areas such as Marmot basin back-country and the Maligne range.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A dusting of new snow covers old hard wind slabs, and scoured surfaces in the ALP and exposed areas of TL. Cold temps have created a weak, faceted upper snowpack. Wind slabs have been most reactive on solar aspects, where crusts are buried. The Jan 17 SH is down 50-70cm at TL and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-45cm of snow in the past 48h with moderate SW winds have created reactive soft slabs. These new storm slabs sit over a variety of wind affected surfaces including pockets of Windslab near ridgetop. The Midpack is strong in deep snowpack areas but this increase in loading will stress the weak, facetted basal snowpack. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 40 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of intense solar radiation and most notably, sustained cold temperatures promoting faceting. Down 50 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of intense solar radiation and most notably, sustained cold temperatures promoting faceting. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Cold temperatures have faceted the upper snowpack, leaving no slab over a weakness down 40cm (surface hoar, facets, and/or crust). However, the stronger mid-pack could act as a slab over weak depth hoar, which comprises the lower third of the snowpack. This is pronounced in shallow areas such as Marmot basin back-country and the Maligne range.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A dusting of new snow covers hard wind slabs and scoured surfaces in the alpine and exposed areas at tree line. Cold temperatures have created a weak and faceted upper snowpack. Wind slabs have been most reactive on solar aspects where crusts are buried. The Jan 17 surface hoar is down 50-70cm at TL and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 40 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of intense solar radiation and most notably, sustained cold temperatures promoting faceting. Down 50 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of solar radiation and most notably, sustained cold temperatures promoting faceting. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Cold temps have faceted the upper snowpack leaving a weak slab over a faint instability down 40cm (surface hoar/facets on a crust). Look for areas where a strong mid-pack will support a rider over the deep persistent weakness. A shallower mid-pack will act as a slab if triggered, sliding on facets and depth hoar in the lower third of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A dusting of new snow covers hard wind slabs and scoured surfaces in the alpine and exposed areas at tree line. Cold temperatures have created a weak and faceted upper snowpack. Wind slabs have been most reactive on solar aspects where crusts are buried. The Jan 17 surface hoar is down 50-70cm at TL and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of solar radiation and most notably, sustained cold temperatures promoting faceting. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of solar radiation and most notably, sustained cold temperatures promoting faceting. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Cold temps have faceted the upper snowpack leaving a weak slab over a instability of surface hoar/facets on a crust down 40cm. The thicker spots have a strong mid-pack and bridges the deep persistent basal weakness of depth hoar. A thinner snow-pack can act as a slab initiating the basal facets and depth hoar in the lower part of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of storm snow covers hard wind slabs in the alpine and exposed areas of tree line. In sheltered areas at and below tree line the storm snow is covering surface hoar and facets. The Jan 17 surface hoar is down 50-70cm at TL and below. the mid and lower snowpack is well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25-40cm of recent snow formed windslabs from moderate SW winds over the past week that are now buried and difficult to identify. More recent N winds have also formed slabs immediately below ridge crests. The midpack is strong in deep snowpack areas but this increase in loading will stress the weak, facetted basal snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. This has been affected by variable winds, isolated periods of solar radiation and most notably, sustained cold temperatures promoting faceting. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. Recent new snow has been affected by Light to Moderate westerly winds. Cold conditions continue promoting faceting of the snowpack. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack is faceted creating a weak slab over a instability of surface hoar/facets on a crust down 40cm. The thicker snowpack spots have a strong mid-pack bridging the deep persistent basal weakness of depth hoar. Thinner snow-pack zones are much less consolidated and can act as a slab triggering the basal depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of storm snow covers old hard wind slabs in the alpine and exposed areas of tree line. In sheltered areas at and below tree line the storm snow is covering surface hoar and near surface facets. The Jan 17 surface hoar is down 50-70cm at TL and below. the mid and lower snowpack is well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. Recent new snow has been affected by Light to Moderate westerly winds. Cold conditions continue promoting faceting of the snowpack. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. Recent new snow has been affected by light to moderate westerly winds. Cold conditions continue promoting faceting of the snowpack. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline and below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack is faceted creating a weak slab over a faint, inconsistent layer of surface hoar/facets on a crust down 40cm. The thicker snowpack spots have a strong mid-pack bridging the deep persistent basal weakness of depth hoar. Thinner snow-pack zones are much less consolidated and can act as a slab triggering the basal depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5cm in the past 24hrs brings the weekly total to 20cm which covers old wind slabs in the alpine and exposed areas of tree line. In sheltered areas at tree line and below the storm snow is covering surface hoar and near surface facets. The mid and lower snowpack is well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50 cm of snow has fallen since Feb 2. Recent new snow has been affected by light to moderate westerly winds. Cold conditions continue promoting faceting of the snowpack. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline and below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Great variability is found in the snowpack in the alpine and near treeline. Deep facets, windslab, suncrust, and snow depths from 0-200+ cm are all present. Midpack surface hoar can be found in isolated locations at treeline and below, and is producing hard but sudden test results. A weak basal snowpack exists in many areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack is faceted creating a weak slab over a faint, inconsistent layer of surface hoar/facets on a crust down 40cm. The thicker snowpack spots have a strong mid-pack bridging the deep persistent basal weakness of depth hoar. Thinner snow-pack zones are much less consolidated and can act as a slab triggering the basal depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of settled snow covers old wind slabs in the alpine and exposed areas at tree line. In sheltered areas at tree line and below the recent snow is covering surface hoar and facets. The mid and lower snowpack is well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of new snow has buried previous windslabs on all aspects. The midpack remains strong in deep snowpack areas, but may act as a slab above deep weak layers in shallower areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent new snow has been affected by Light to Moderate westerly winds. Cold conditions continue promoting faceting of the snowpack. Down 30 to 75cm, Jan 17 surface hoar produces sudden planar shears in isolated locations treeline an below. A weak basal snowpack exists in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At treeline and above a mix of powder, weak surface facets, wind slab, and some sun crust, can be found over a supportive mid-pack. In isolated areas at treeline and below the Jan 17 surface hoar can be found down 30-60 cm, and is producing hard but sudden test results. Weak basal facets can be found in thinner snow pack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack is faceted creating a weak slab over a faint, inconsistent layer of surface hoar/facets on a crust down 40cm. The thicker snowpack spots have a strong mid-pack bridging the deep persistent basal weakness (depth hoar). Thinner snow-pack zones are much less consolidated, where the midpack may act as a slab on the basal depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of settled snow on old wind slabs in the alpine. In sheltered areas the recent snow is covering surface hoar and facets. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong. Wind and new snow will likely create isolated soft slabs by tomorrow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At treeline and above a mix of powder, weak surface facets, wind slab, and some sun crust, can be found over a supportive mid-pack. In isolated areas at treeline and below the Jan 17 surface hoar can be found down 30-60 cm, and is producing hard but sudden test results. Weak basal facets can be found in some thin areas of the Little Yoho region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 40 cm has accumulated since Feb 1 along with isolated crusts on steep solar slopes and wind effect treeline and above. In isolated areas at treeline and below the Jan 17 surface hoar can be found down 30-60 cm, and is producing hard but sudden test results. Weak basal facets can be found in thinner snow pack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Fresh windslabs have formed in exposed terrain, lee to SW then N winds.  Remnants of a surface hoar layer (Jan 18) down 40cm could be reactive in isolated areas treeline and below. A strong midpack exists in thick snowpack areas, but is weaker in thinner snow-pack zones over weak basal depth hoar, consistently giving hard, sudden results in  tests. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A dusting of new snow fell overnight. 15cm of settled snow resides on old wind slabs in the alpine. In sheltered areas the recent snow is covering surface hoar and facets. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong. A dusting of new snow .</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The midpack remains strong in deep snowpack areas, but is acting as a slab above deep weak layers in shallower areas that is reactive skiers </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/9a62c08f-08dc-4822-9a9f-005dab6ae96d" target="_blank"><span class="s_9255B882">mainly at below treeline elevations</span></a><span class="s_AA239A9B"> where melt freeze crusts have been preserved. Continued snowfall on Saturday is burying windslabs formed by recent Westerly winds. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 40 cm has accumulated since Feb 1 along with isolated crusts on steep solar slopes and wind effect treeline and above. In isolated areas at treeline and below the Jan 17 surface hoar can be found down 30-75 cm, and is producing hard but sudden test results. Weak basal facets can be found in thinner snow pack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 40 cm has accumulated since Feb 1 along with isolated crusts on steep solar slopes and wind effect treeline and above. In isolated areas at treeline and below the Jan 17 surface hoar can be found down 30-60 cm, and is producing hard but sudden test results. Weak basal facets can be found in thinner snow pack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Towards the Icefields, the alpine is wind affected. The Jan 18 surface hoar layer (down 40cm) has faceted away in most places, but shows isolated sensitivity at treeline and below in the Icefields region. The midpack is mainly supportive, over depth hoar in shallow areas. Although structurally weak, this layer has been generally dormant lately.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of settled snow resides on old wind slabs in the alpine. In sheltered areas the recent snow is covering surface hoar and facets. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong. Surface faceting is softening old ski tracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 40 cm has accumulated since Feb 1 along with isolated crusts on steep solar slopes and wind effect treeline and above. In isolated areas at treeline and below the Jan 17 surface hoar can be found down 30-60 cm, and is producing hard but sudden test results. Weak basal facets can be found in thinner snow pack areas.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of loose facets sitting over an old layer of surface hoar and crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Towards the Icefields, the alpine is wind affected. The Jan 18 surface hoar layer (down 40cm) has faceted away in most places, but shows isolated sensitivity at treeline and below in the Ice fields region. The midpack is mainly supportive, over depth hoar in shallow areas. Although structurally weak, this layer has been generally dormant lately.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of settled snow resides on old wind slabs in the alpine. In sheltered areas the recent snow is covering surface hoar and facets. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong. Surface faceting is softening old ski tracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The upper snowpack is highly variable with a variety of Windslab and Wind affect in all but the most protected areas. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The midpack remains strong in deep snowpack areas, but is acting as a slab above deep weak layers in shallower areas that is reactive skiers </span><a href="https://www.avalanche.ca/map?panel=mountain-information-network-submissions/9a62c08f-08dc-4822-9a9f-005dab6ae96d" target="_blank"><span class="s_9255B882">mainly at below treeline elevations</span></a><span class="s_AA239A9B"> where melt freeze crusts have been preserved. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of loose facets sitting over an old layer of surface hoar and crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of loose facets sitting over an old layer of surface hoar and crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack continues to lose cohesion from facetting. Wind effect is visible in open terrain from previous SW switching to N winds. The Jan 18 layer (down 40cm) has faceted away in most places, but shows isolated sensitivity at treeline and below in the Icefields region. The midpack is mainly supportive, over depth hoar in shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of settled, faceted snow resides on old wind slabs in the alpine. N'ly winds have deposited thin wind slabs on SE-SW aspects at ridge-top. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong. Surface faceting is softening old ski tracks.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of loose facets sitting over an old layer of surface hoar and crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of  very loose facets sitting over an old layer of surface hoar &amp; crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack on solar aspects could be stiffening up, otherwise remains faceted. Wind effect is visible in open terrain from previous SW switching to N winds. The Jan 18 layer (down 40cm) has faceted away in most places, but shows isolated sensitivity at treeline and below. The midpack is mainly supportive, over depth hoar in shallow areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of settled, faceted snow resides on old wind slabs in the alpine. Northerly winds have deposited thin wind slabs on SE-SW aspects at ridge-top. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong. Surface faceting is softening old ski tracks.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of very loose facets sitting over an old layer of surface hoar &amp; crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of loose facets sitting over an old layer of surface hoar and crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack on solar aspects is stiffening up otherwise it remains faceted on polar aspects. Wind effect is in open terrain from previous SW switching to N winds. The Jan 18 layer of surface hoar/facets  down 40cm has mostly faceted away, yet still shows isolated sensitivity at treeline and below. The midpack is supportive over depth hoar. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of settled, faceted snow resides on old wind slabs in sheltered areas. Moderate to strong  winds have deposited thin wind slabs on exposed terrain features at ridge-top. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> A couple centimeters of new snow has covered a variety of wind affected surfaced at all elevations including windslabs on all aspects in the Alpine and at Treeline. The midpack is generally strong in thick snowpack locations, and is bridging weak basal facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is stable, but with each passing day it becomes weaker and more unconsolidated as the cold temperatures facet the surface layers. Surface conditions are a mix of wind effect or 30 cm of loose facets sitting over an old layer of surface hoar and crust (Jan 17) down 40-60 cm. Snowpack tests show hard, resistent shears on this layer. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temperatures continue to weaken the surface snow. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack remains faceted on all aspects. Wind effect in open terrain from previous SW and now N winds. Much of the mid-pack is faceted with some strength and support on skis but not under foot. Isolated sensitivity to Jan 18th layer at treeline and below, but not consistent to all areas. Large depth hoar on the ground at all locations. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of settled, faceted snow resides on old wind slabs in sheltered areas. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed areas BTL. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temperatures continue to weaken the surface snow. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temperatures continue to weaken the surface snow. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack remains faceted on all aspects. Wind effect in open terrain from previous SW and now N winds. Much of the mid-pack is faceted with some strength and support on skis but not always under foot. Isolated sensitivity to Jan 18th layer at treeline and below, but not consistent to all areas. Large depth hoar on the ground, everywhere. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of settled, faceted snow resides on old wind slabs in sheltered areas. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed areas BTL. A crust on steep solar aspects makes for difficult traveling conditions, both uphill and down. The mid and lower snowpack is well settled and strong.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temperatures continue to weaken the surface snow. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack remains faceted on all aspects. Wind effect in open terrain from previous SW and now N winds. Much of the mid-pack is faceted with some strength and support on skis but not always under foot. Isolated sensitivity to Jan 18th layer at treeline and below, but not consistent to all areas. Large depth hoar on the ground, everywhere. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Expect surface facets and a variety of windslab in most locations. Sun crust will be found on steeper solar terrain making for difficult travel. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed treeline areas. The mid and lower snowpack is well settled and strong. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack remains faceted on all aspects. S and W aspects are starting to show signs of solar input. Wind effect in open terrain from previous SW and now N winds. Much of the mid-pack is faceted with some strength and support on skis but not always under foot. The warming trend on Wednesday will destabilize the snowpack.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Expect surface facets and a variety of windslab in most locations. Sun crust will be found on steeper solar terrain making for difficult travel. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed treeline areas. The mid and lower snowpack is well settled and strong. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of powder is covering variety of wind affected surfaces at all elevations including old windslabs on all aspects in the Alpine and at Treeline. This loose snow will form new windslabs with increasing wind beginning Tuesday night. The midpack is generally strong in thick snowpack locations, and is bridging weak basal facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">The warming trend will destabilize the upper snowpack, particularly where exposed to the sun.  The upper snowpack remains generally facetted, but the surface has been sun affected on solar aspects. Wind effect is visible in open terrain from previous SW switching to N winds. The mid and lower snowpack is facetted but still generally carries skis. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Expect surface facets and a variety of wind slabs in most locations. Sun crusts will be found on steeper solar terrain making for difficult travel. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed treeline areas. The mid and lower snowpack is well settled and strong. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Despite the weakening slab above it, Jan 17 surface hoar lingers down 40-60 cm in isolated locations and produces hard, resistent shears. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened and facetted the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">10cm of new snow through Thursday and moderate winds could create new windslabs in the alpine. New snow will bury a variety of surface; surface hoar, facets and crusts. The upper snowpack remains generally facetted. The mid and lower snowpack is facetted but still generally carries skis. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Expect a variety of surface conditions from surface facets to wind slabs, and sun crusts . Sun crusts will be found on steeper solar terrain making for difficult travel. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed treeline areas. The mid and lower snowpack is well settled and strong. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened and facetted the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened and facetted the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">10cm of new snow through Friday and moderate winds could create new windslabs in the alpine. New snow will bury a new surface hoar layer, facets and crusts. The upper snowpack remains generally facetted. The mid and lower snowpack is facetted but still generally carries skis. Below treeline warmer daytime temps will weaken the snowpack.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">3cm of new snow covers surface facets, wind slabs, and sun crusts . Sun crusts will be found on steeper solar terrain making for difficult travel. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed treeline areas. The mid and lower snowpack is well settled and strong. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds with extreme gusts contributing to Windslab development on Thursday. These new Windslabs sit over 10-15 cm of faceted powder in the alpine and at treeline. Surface snow below treeline is mostly unaffected by wind. The midpack is generally strong in thick snowpack locations, and is bridging weak basal facets.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Prolonged cold temperatures have weakened and facetted the upper snowpack. Wind effect is common in the alpine and several recent crusts can be found on steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">A trace to 20 cm of new snow came with moderate to strong SW-W winds. This sits over weak surface facets, previous wind effect and crusts isolated to steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_1681A555 { font-family: 'Times New Roman';font-style: Normal;font-weight: normal;font-size: 16px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">2-5cm new snow Thursday night, with Moderate SW winds, has generally had little affect on the snowpack.  Isolated small windslabs could, however, exist in Maligne area.  The upper snowpack remains faceted; sluffing in steep terrain may be possible with ski traffic or strong sun. A strong midpack overlies the (dormant) basal weakness.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of new snow covers surface facets, wind slabs, and sun crusts . Sun crusts will be found on steeper solar terrain making for difficult travel. Moderate to strong winds have deposited thin wind slabs on exposed terrain features at ridge-top and exposed treeline areas. The mid and lower snowpack is well settled and strong. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A trace to 20 cm of new snow came with moderate to strong SW-W winds. This sits over weak surface facets, previous wind effect and crusts isolated to steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A trace to 20 cm of new snow came with moderate to strong SW-W winds. This sits over weak surface facets, previous wind effect and crusts isolated to steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">While much of the upper snowpack remains dry and faceted, dramatic seasonal temperature swings have begun a diurnal melt-freeze cycle to surface snow, especially steep southern aspects, BTL; but possible on all solar aspects and elevations. The mid pack remains strong enough to support a rider, but may be weak underfoot.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 12cm brings the storm snow total to ~30cm which now covers surface facets and sun crusts. The West end of the Park saw twice as much snow yesterday as the East side. Moderate southerly winds have deposited pockets of wind slab along ridge lines and cross loaded features. The mid and lower snowpack is well settled and strong. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A trace to 20 cm of new snow came with moderate to strong SW-W winds. This sits over weak surface facets, previous wind effect and crusts isolated to steep solar slopes. Weaker layers like the Jan.17 surface hoar/facets linger down 40-60 cm in some locations, but are currently lying dormant. A weak basal snowpack exists in thin snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15 cm of recent snow with moderate to strong SW-W winds has formed thin slabs in open areas above treeline. This snow sits over either weak facets, previous wind effect or sun crusts on steep solar aspects. The mid pack varies from supportive in thicker snowpack areas to weak and completely faceted in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The snowpack remains mainly dry and faceted. The mid pack is relatively strong for the region, and supportive to skis in most areas. Isolated surface hoar still exists at/below tree line, South of the Icefields. A thin sun crust has been observed below tree line on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">~30cm of recent snow covers 20-30cm of facets and/or sun crusts up to 3cm thick. Recent moderate southerly winds have deposited isolated pockets of wind slab along ridge lines and cross loaded features. The mid and lower snowpack is well settled and strong. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15 cm of recent snow with moderate to strong SW-W winds has formed thin slabs in open areas above treeline. This snow sits over either weak facets, previous wind effect or sun crusts on steep solar aspects. The mid pack varies from supportive in thicker snowpack areas to weak and completely faceted in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds Monday have redistributed recent snow into wind slabs in open areas above treeline. This recent snow sits over weak facets, previous wind effect or sun crusts on steep solar aspects. The mid pack varies from supportive in thicker snowpack areas to weak and completely faceted in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">New snow accumulating over a variety of old surfaces (loose facets in sheltered terrain, wind affected in exposed areas, sun crust to treeline to solar aspects) . The mid pack is relatively strong for the region, supportive to skis in most areas. Isolated surface hoar is still reactive at/below tree line, South of the Icefields. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">~30cm of recent snow covers 20-30cm of facets, wind slabs, and/or sun crusts up to 3cm thick. Recent moderate southerly winds have deposited isolated pockets of wind slab along ridge lines and cross loaded features. The mid and lower snowpack is well settled and strong. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds Monday have redistributed recent snow into wind slabs in open areas above treeline. This recent snow sits over weak facets, previous wind effect or sun crusts on steep solar aspects. The mid pack varies from supportive in thicker snowpack areas to weak and completely faceted in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds overnight Monday have redistributed recent snow into wind slabs in open areas above treeline. This recent snow sits over weak facets, previous wind effect or sun crusts on steep solar aspects. The mid pack varies from supportive in thicker snowpack areas to weak and completely faceted in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Up to 15cm of new snow came in with strong to extreme SW winds. Previous old surfaces were; loose facets in sheltered terrain; wind affected in exposed areas; and, sun crust to treeline on solar aspects. The mid/lower snowpack is relatively strong for the region in deeper snowpack areas, and weak and facetted in shallow snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 25cm of new snow brings our storm total to approximately 50cm at Tree Line. Light to moderate winds have formed soft slabs on lee aspects and cross loaded terrain features. The storm snow overlies a plethora of old surfaces including; sun crusts on solar aspects, hard wind slab in exposed areas, and surface facets in sheltered locations. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds overnight Monday have redistributed recent snow into wind slabs in open areas above treeline. This recent snow sits over weak facets, previous wind effect or sun crusts on steep solar aspects. The mid pack varies from supportive in thicker snowpack areas to weak and completely faceted in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30cm recent low density snow (higher amounts in western regions) over previously wind blown surfaces in the alpine, and 30-50cm of facets below. Lower elevations are completely faceted to ground. Steep areas continue to produce sluffing in many areas with buried suncrust on steep S aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Windslabs in the alpine and treeline on N-E aspects. Previous old surfaces were; loose facets in sheltered terrain; wind affected in exposed areas; and, sun crust to treeline on solar aspects. The mid/lower snowpack is relatively strong for the region in deeper snowpack areas, and weak and facetted in shallow snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Roughly 50cm of snow has fallen at tree-line over the last week. Moderate winds and mild temp's have created a cohesive soft slab which sits on a plethora of old surfaces including; sun crusts on solar aspects; hard wind slab in exposed areas; and surface facets in sheltered locations. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30cm recent low density snow over previously wind blown surfaces in the alpine, and 30-50cm of facets below. In little Yoho the snowpack is generally thicker and settled, except for thin areas which have facets to ground. Steep areas continue to produce sluffing in many areas with buried suncrust on steep S aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30cm recent low density snow (higher amounts in western regions) over previously wind blown surfaces in the alpine, and 30-50cm of facets below. Lower elevations are completely faceted to ground. Steep areas continue to produce sluffing in many areas with buried suncrust on steep S aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Windslabs located in the alp and TL on N to E aspects. The snowpack is relatively strong through most of the region especially in deep snowpack areas. Shallow areas are weak, and will morph quickly to moist 'spring like' slab conditions from the surface down. With the persistent basal weakness, this could fail with the full depth of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Roughly 50cm of snow has fallen at tree-line over the last week. Moderate winds and mild temp's have created a cohesive soft slab which sits on: a sun crust on solar aspects; hard wind slab in exposed areas; and surface facets in sheltered locations. Steep solar aspects (SE through to W) now have a crust from yesterday's sunshine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20cm of powder is being blown into new wind slabs by moderate west winds. This is sitting on a sun crust on steep south aspects and hard wind affected surfaces everywhere else that are providing a good sliding surface for the new snow. Crust facet combinations remain deep in the snowpack at lower elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30cm recent low density snow (higher amounts in western regions) over previously wind blown surfaces in the alpine, and 30-50cm of facets below. Lower elevations are completely faceted to ground. Steep areas continue to produce sluffing in many areas with buried suncrust on steep S aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15- 40cm has accumulated since March 7. Modertate to strong SW-W winds have redistributed this snow treeline and above. This snow sits over previous widespread wind effect in the alpine, suncrusts on steep S aspects and 30-50cm of sugary facets everywhere else. While a tough midpack exists in thicker areas, facets to ground are seen in many others.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Moist surface snow treeline and below and the alpine is heavily wind effected. Deep snowpack areas are relatively strong through most of the region. Shallow areas are weak, and will morph quickly to moist 'spring like' slab conditions from the surface down. With the persistent basal weakness, this could fail with the full depth of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">17cm of low density snow fell overnight at treeline. It overlies a soft storm slab in most areas, and on steep solar aspects (SE-W) a sun crust. The storm slab is up to 50cm deep and has been reactive to skier triggering. The storm slab sits on a sun crust on solar aspects; hard wind slab in exposed areas; and surface facets in sheltered locations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15- 40cm has accumulated since March 7. Modertate to strong SW-W winds have redistributed this snow treeline and above. This snow sits over previous widespread wind effect in the alpine, suncrusts on steep S aspects and 30-50cm of sugary facets everywhere else. While a tough midpack exists in thicker areas, facets to ground are seen in many others.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15- 50cm has accumulated since March 7. Modertate to strong SW-W winds have redistributed this snow treeline and above. This snow sits over previous widespread wind effect in the alpine, suncrusts on steep S aspects and 30-50cm of sugary facets everywhere else. While a tough midpack exists in thicker areas, facets to ground are seen in many others.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Moist surface snow treeline and below and the alpine is heavily wind effected. Deep snowpack areas are relatively strong through most of the region. Shallow areas are weak, and will morph quickly to moist 'spring like' slab conditions from the surface down. With the persistent basal weakness, this could fail with the full depth of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On solar aspects, sun crusts are buried 15cm and 50cm and are several centimeters thick. Moderate southerly winds have redistributed the recent 50-60 cm of storm snow, which sits on a sun crust on solar aspects, hard slab in exposed areas, and facets in sheltered locations. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15- 50cm has accumulated since March 7. Modertate to strong SW-W winds have redistributed this snow treeline and above. This snow sits over previous widespread wind effect in the alpine, suncrusts on steep S aspects and 30-50cm of sugary facets everywhere else. While a tough midpack exists in thicker areas, facets to ground are seen in many others.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and moist snow at lower elevations. 15-50 cm of snow has accumulated since March 7. This sits over a mix of facets, sun crust and wind slabs above treeline, and over 30-50 cm of weak facets elsewhere. While a supportive mid-pack exists in thicker areas, weak facets to the ground are seen in many thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Moist surface snow treeline and below and the alpine is heavily wind effected. Deep snowpack areas are relatively strong through most of the region. Shallow areas are weak, and will morph quickly to moist 'spring like' slab conditions from the surface down. With the persistent basal weakness, this could fail with the full depth of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface snow consists of sun crust on solar aspects and loose dry snow on polar aspects. This past weeks snow has settled into a 50cm soft slab which sits on a sun crust, hard slab in exposed areas, and facets in sheltered locations. The snowpack is generally facetted from Feb's cold streak and could loose strength quickly with the warming temps.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind slabs formed on Thursday and Friday and loose snow in sheltered areas are sitting on a sun crust on steep south aspects, facets in sheltered areas, and hard wind affected surfaces everywhere else. The lower snowpack remains weak and facetted, and as the warm temperatures continue there is a possibility this layer could produce large avalanches</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and moist snow at lower elevations. 15-50 cm of snow has accumulated since March 7. This sits over a mix of facets, sun crust and wind slabs above treeline, and over 30-50 cm of weak facets elsewhere. While a supportive mid-pack exists in thicker areas, weak facets to the ground are seen in many thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and moist snow at lower elevations. 15-50 cm of snow has accumulated since March 7. This sits over a mix of facets, sun crust and wind slabs above treeline, and over 30-50 cm of weak facets elsewhere. While a supportive mid-pack exists in thicker areas, weak facets to the ground are seen in many thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The snowpack remains dry on polar (shady) aspects, at treeline &amp; alpine elevations. Elsewhere (solar aspects) it is quickly transitioning to Spring. Thin overnight crust recovery, breaking down quickly daily. Isothermal snowpack Below Treeline on solar aspects. As the snowpack warms, the Deep Persistent layers may become active on polar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface snow consists of sun crust on solar aspects and loose dry snow on polar aspects. A ~50cm soft slab sits on a variety of old surfaces: sun crust on solar aspects; hard slab in exposed areas; and facets in sheltered locations. The snowpack is generally facetted from Feb's cold streak and could lose strength quickly with the warming temps.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The upper snowpack consists of recent wind slabs over facetted wind affected surfaces on shaded slopes, and moist snow on solar aspects. The lower snowpack remains weak and facetted, and as the warm temperatures continue there is a possibility this layer could produce large avalanches</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and moist snow at lower elevations. 15-50 cm of snow has accumulated since March 7. This sits over a mix of facets, sun crust and wind slabs above treeline, and over 30-50 cm of weak facets elsewhere. While a supportive mid-pack exists in thicker areas, weak facets to the ground are seen in many thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and moist snow at lower elevations. 10-20 cm of recent snow sits over a mix of facets, sun crust and wind slabs above treeline, and over 30-50 cm of weak facets elsewhere. While a supportive mid-pack exists in thicker areas, weak facets to the ground are seen in many thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is undergoing rapid changes as it transitions from Winter to Spring. Isothermal conditions are present at lower elevations, accompanied by melt freeze/sun crusts on all but true North aspects in the Alpine. Temps did not go below freezing last night at higher elevations! And a ~40cm slab exists in the Alpine and at Tree Line. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and moist snow at lower elevations. 10-20 cm of recent snow sits over a mix of facets, sun crust and wind slabs above treeline, and over 30-50 cm of weak facets elsewhere. While a supportive mid-pack exists in thicker areas, weak facets to the ground are seen in many thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and isothermal snow at lower elevations. Above treeline, 10-50 cm of recent snow sits over a mix of facets, sun crust and wind slabs.  While a supportive mid-pack exists in thicker areas, very weak facets to the ground are seen in many thinner areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Spring like snowpack on solar aspects, with minimal crust recovery overnight rapidly breaking down with daily intense solar input. The entire snowpack is isothermal below treeline on solar aspects. The snowpack remains dry on shady aspects at upper elevations, but may become reactive with continued warm temps.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Spring snowpack on solar aspects, with minimal crust recovery overnight rapidly breaking down under daily intense solar input. The entire snowpack is isothermal below treeline on solar aspects. The snowpack remains dry on shady aspects at upper elevations, but may become reactive with continued warm temps.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A ~40cm slab exists at alpine and tree-line elevations, while isothermal conditions are present below tree-line. Surface crusts of varying hardness are prevalent on all but true North aspects in the Alpine. A second night in a row of above freezing temp's at tree-line elevation has prevented a solid crust from forming at 2000m and above.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts or moist snow on solar aspects and isothermal snow at lower elevations. Above treeline,10-50 cm of recent snow sits over a mix of facets, sun crust and wind slabs. While a supportive mid-pack exists in thicker areas, very weak facets to the ground are seen in many thinner areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On all aspects and elevations except high north, morning surface crusts are deteriorating early in the day and the snowpack is becoming wet with isothermal snow at low elevations. North aspects in alpine areas are holding some dry snow, but the warm air temperatures may have created soft slab conditions overlying weak facets formed in February.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Spring snowpack on solar aspects, with minimal crust recovery overnight rapidly breaking down under daily intense solar input. The entire snowpack is isothermal below treeline on solar aspects. The snowpack remains dry on shady aspects at upper elevations, but may become reactive with continued warm temps.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A ~40cm slab exists at alpine and tree-line elevations, while isothermal conditions are present below tree-line. Surface crusts of varying hardness are prevalent on all but true North aspects in the Alpine. A THIRD night in a row of above freezing temps at tree-line elevation has prevented a solid crust from forming at 2000m and above.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar affect is the primary concern for Friday. Up to 1m of moist snow on solar aspects during the heat of the day. The lower snowpack remains weak and facetted, and as the warm temperatures continue there is a possibility this layer could produce large avalanches.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On all aspects and elevations except high north, morning surface crusts are deteriorating early in the day and the snowpack is becoming wet with isothermal snow at low elevations. North aspects in alpine areas are holding some dry snow, but the warm air temperatures may have created soft slab conditions overlying weak facets formed in February.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We are moving towards a spring snowpack with isothermal releases in thin areas and on sun-exposed slopes. Risk is greatly reduced by finishing the day early before things heat up. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">As of Friday afternoon there is wet surface snow on solar aspects at treeline and alpine, unsupportive slush below treeline. As the temperatures start to cool on Saturday expect a melt freeze crust where surface snow was previously moist. The snowpack remains dry on shady aspects at upper elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A ~40cm slab exists at alpine and tree-line elevations over facets and suncrust. Above freezing temperatures all week at and above 2000m have resulted in poor overnight recovery of the snow surface. Isothermal conditions below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We are moving towards a spring snowpack with isothermal releases in thin areas and on sun-exposed slopes. Risk is greatly reduced by finishing the day early, before things heat up. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar aspects have a melt freeze crust which is deteriorating as the day warms up. Dry powder is still found on high north aspects, where a 20-50 cm settlement slab overlays the March 7th facets. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Wet surface snow (top 10cm) on all aspects below 1800m. Temperatures start to cool on Saturday evening and you can expect a weak melt freeze crust where snow was previously moist; this may break-down BTL over the day Sunday.  The snowpack has remained dry on shady aspects on higher elevations and may be best chance at good riding in the short term.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High freezing levels all week have resulted in poor overnight recovery of the snow surface. Isothermal conditions exist below tree line. Expect to find supportive/breakable crust on all aspects at and below tree line and on steep solar aspects in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar aspects have a melt freeze crust which is deteriorating as the day warms up. Dry powder is still found on high north aspects, where a 20-50 cm settlement slab overlays the March 7th facets. Many areas exhibit a cohesive midpack with little sign of basal weak layers, while other thin areas have weak facets to the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar aspects have a melt freeze crust which is deteriorating with daytime warming. Dry snow is still found on high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Wet surface snow (top 10cm) on all aspects below 1800m. Temperatures start to cool on Saturday evening and you can expect a weak melt freeze crust where snow was previously moist; this may break-down BTL over the day Sunday. The snowpack has remained dry on shady aspects on higher elevations and may be best chance at good riding in the short term.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High freezing levels all week have resulted in poor overnight recovery of the snow surface. Expect to find a breakable crust in the morning on all aspects at and below tree line and for the crust to break down into moist snow by the afternoon. </span><a href="https://avalanche.org/avalanche-encyclopedia/isothermal/" target="_blank"><span class="s_9255B882">Isothermal</span></a><span class="s_AA239A9B"> conditions exist below tree line. Cool dry snow exists on high Northerly aspects</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar aspects have a melt freeze crust which is deteriorating with daytime warming. Dry snow is still found on high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Overnight cooling has developed a melt freeze crust on all aspects and elevations except for hight north facing terrain. This crust has been deteriorating with daytime warming. Dry snow is still found on high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The entire snowpack is isothermal below treeline, and higher on solar aspects. A surface crust is forming overnight and breaking down with daytime warming/solar input.  The snowpack has remained dry on shady aspects at higher elevations - in deep areas it is generally well settled and bonded, in shallow areas it is facetted and unsupportive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High freezing levels all week have resulted in poor overnight recovery of the snow surface. Expect to find a breakable crust in the morning on all aspects at and below tree line and for the crust to break down into moist snow by the afternoon. </span><a href="https://avalanche.org/avalanche-encyclopedia/isothermal/" target="_blank"><span class="s_9255B882">Isothermal</span></a><span class="s_AA239A9B"> conditions exist below tree line. Cool dry snow exists on high Northerly aspects</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack structure varies greatly with aspect, elevation and time of day. We received 2-5 mm of precipitation over the weekend with a 1600m freezing level.  New snow sits over a 4cm melt freeze crust on solar aspects above 1700m. Pockets of dry snow over windslab still exist on north aspects above TL. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Midpack is strong above 1700m &amp; Isothermic BTL.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Overnight cooling has developed a melt freeze crust on all aspects and elevations except for hight north facing terrain. This crust has been deteriorating with daytime warming. Dry snow is still found on high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some wind and fresh snow will create new windslabs near ridge crests and in open lee areas. Dry snow is still found on high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Cool temps and cloudy skies reducing the diurnal(daily) swings in snowpack instability. The entire snowpack is isothermal below treeline. The snowpack has remained dry on shady aspects at higher elevations - in deep areas it is generally well settled and bonded, in shallow areas it is facetted and unsupportive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Temperatures have dipped below 0 at treeline and above for the first time in a week. Expect to find a variable crust in the morning, which may break down into moist snow by the afternoon. </span><a href="https://avalanche.org/avalanche-encyclopedia/isothermal/" target="_blank"><span class="s_9255B882">Isothermal</span></a><span class="s_AA239A9B"> conditions exist below tree line. Cool dry snow exists on high Northerly aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some wind and fresh snow will create new windslabs near ridge crests and in open lee areas. Dry snow is still found on high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of new snow overlays a variate of surfaces depending on aspects and elevations. A supportive melt freeze crust is present below this new snow in most areas excluding high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">5-25cm of new snow (more in the Jasper area than near the Icefields), was redistributed by moderate N winds in the alpine, is settling fast and generally bonding well to previous surfaces. The entire snowpack is isothermal below treeline. On shady alpine aspects the snowpack remains dry.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Flurries delivered 10-15cm of snow to the alpine yesterday. SW winds redistributed this into thin soft slabs at alpine and tree-line lee features. Cooler temps overnight will have created a supportive crust to carry a person on skis, but this will likely break down by mid-day into isothermal, oatmeal-like slop from 2000m and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of new snow overlays a variate of surfaces depending on aspects and elevations. A supportive melt freeze crust is present below this new snow in most areas excluding high north aspects. Many areas exhibit a cohesive midpack over the basal facets, while other thin areas have weak facets to the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent snow overlies a variety of surfaces depending on aspect and elevation. A supportive melt freeze crust is present below the new snow in most areas excluding high north aspects. Many areas have a cohesive mid-pack over the basal facets, while thin areas often have weak facets to ground. Lower elevations are becoming isothermal. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">New snow is settling fast and generally bonding well to previous surfaces. The snowpack is cycling from isothermal, to overnight freeze with an inconsistent, supportive crust below (about 10cm thick) at treeline on all aspects. Crust breaking down by mid-morning on all solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 to 15cm of recent snow has been redistributed by SW winds into thin soft slabs at alpine and tree-line lee features. Freezing levels are dropping to valley bottom at night, creating a supportive crust to travel on. The crust was observed to break down by mid-afternoon on solar aspects steeper than 25 degrees. Dry snow is found on N'ly aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of recent snow (10-20cm in the front ranges) is sitting on a thick supportive crust in most locations, and appears to be bonding well. Steep north facing alpine terrain is still holding dry snow. The midpack is well settled, and basal weaknesses persist at treeline and in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent snow overlies a variety of surfaces depending on aspect and elevation. A supportive melt freeze crust is present below the new snow in most areas excluding high north aspects. Many areas have a cohesive mid-pack over the basal facets, while thin areas often have weak facets to ground. Lower elevations are becoming isothermal. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of recent storm snow overlies a supportive melt freeze crust. Some cold North faces and thin areas hold deep facets still. Many areas have a cohesive mid-pack over the basal facets. Lower elevations can become isothermal in the afternoon. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">New snow has settling fast and bonding well to previous surfaces. The snowpack is cycling from isothermal, to overnight freeze with an supportive crust below (about 10cm thick) treeline on all aspects. Crust breaking down under a strong solar influence by mid-morning on any sunny aspect. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We're into the spring melt freeze cycle. At valley bottom the crust this morning was 7cm thick and overlies an isothermal snowpack in most areas. Surface crusts have been breaking down by mid-afternoon on solar aspects steeper than 25 degrees. Dry snow can still be found on N'ly aspects above treeline, and thin soft wind slabs exist on lee slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of recent storm snow overlies a supportive melt freeze crust. Some cold North faces and thin areas hold deep facets still. Many areas have a cohesive mid-pack over the basal facets. Lower elevations can become isothermal in the afternoon. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of recent storm snow overlies a supportive melt freeze crust. Some cold North faces and thin areas hold deep facets still. Many areas have a cohesive mid-pack over basal facets. Lower elevations can become isothermal in the afternoon. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Upper snowpack at TL and below (and alpine solar aspects) have transitioned through a series of deep penetrating and, consistent melt freeze cycles. This seasonal spring rhythm will be less pronounced over the next few days. For now, surface instabilities like wet loose are possible but limited to immediate southern aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We're into the spring melt freeze cycle. At valley bottom the crust this morning was 7cm thick and overlies an isothermal snowpack in most areas. Surface crusts have been breaking down by mid-afternoon on solar aspects steeper than 25 degrees. Dry snow can still be found on N'ly aspects above tree line and thin soft wind slabs exist on lee slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of recent storm snow overlies a supportive melt freeze crust. Some cold North faces and thin areas hold deep facets still. Many areas have a cohesive mid-pack over basal facets. Lower elevations can become isothermal in the afternoon. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where up to 20 cm of soft snow remains from several days ago. By early afternoon the surface crusts are softening with daily warming. There is lingering concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The upper snowpack has transitioned through a series of melt-freeze cycles at at treeline and below on all aspects (and into the alpine on solar aspects). This seasonal spring rhythm is less pronounced over the next few days with cooling temps. On north facing alpine slopes up to 20cm of settled storm snow overlies previous old dry surfaces.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We're into the spring melt freeze cycle. At valley bottom the crust this morning was 7cm thick and overlies an isothermal snowpack in most areas. Surface crusts have been breaking down by mid-afternoon on solar aspects steeper than 25 degrees. Dry snow can still be found on N'ly aspects above tree line and thin soft wind slabs exist on lee slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where up to 20 cm of soft snow remains from several days ago. By early afternoon the surface crusts are softening with daily warming. There is lingering concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where up to 20 cm of soft snow remains from several days ago. By early afternoon the surface crusts are softening with daily warming. There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The snowpack is isothermal at treeline and below on all aspects (and into the alpine on solar) - the upper snowpack in these areas has undergone multiple melt-freeze cycles, a strong crust in the morning will weaken with solar imput/daytime warming. On north facing alpine slopes up to 15cm of settled storm snow overlies previous old dry surfaces.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We are now into a spring melt freeze cycle. We have a strong surface crust this morning, after a cool, clear evening. Surface crusts will break down by mid-afternoon on steep solar aspects, and BTL. Dry snow can still be found on N'ly aspects above tree line and thin soft wind slabs exist on lee slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of moist recent snow along the front ranges is sitting on a thick supportive crust in most locations. In most areas we are seeing a typical spring snowpack with crusts breaking down in the heat of the day. Steep north facing alpine terrain is still holding dry snow. The midpack is generally moist and well settled.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where up to 20 cm of soft snow remains from several days ago. By early afternoon the surface crusts are softening with daily warming. There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where there's up to 20 cm of old soft snow.  There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects and pockets of unconsolidated snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The snowpack is isothermal at treeline and below on all aspects (and into the alpine on solar) - the upper snowpack in these areas has undergone multiple melt-freeze cycles, a strong crust in the morning will weaken with solar input/daytime warming. On north facing alpine slopes up to 15cm of settled storm snow overlies previous old dry surfaces.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The spring melt freeze cycle continues. We have another strong surface crust this morning, expect it to break down this afternoon. The snowpack is isothermal in thin snowpack areas BTL, the mid and lower snow pack is strong at tree line and above, where the HS is over 2m. Dry snow can still be found on Northerly aspects in the high alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where there's up to 20 cm of old soft snow. There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects and pockets of unconsolidated snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where there's up to 20 cm of old soft snow. There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects and pockets of unconsolidated snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Below treeline the snowpack is trending isothermal in the afternoons depending on the overnight freeze. Higher elevations maintains the crust with on-going multiple melt-freeze cycles. On north facing alpine slopes up to 15cm of surface snow overlies previous old dry surfaces.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The spring melt freeze cycle continues. The strong surface crust is unlikely to break down today, with increasing cloud. Below the crust, the snowpack is isothermal in thin snowpack areas BTL. The mid and lower snowpack is strong at tree line and above, where depths are over 2m. Dry snow can be found on Northerly aspects in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is melt-freeze crust on all areas except alpine and treeline north and east aspects where there's up to 20 cm of old soft snow. There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects and pockets of unconsolidated snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Light dusting of snow over a melt-freeze crust on all areas, except alpine and treeline north and east aspects where there's up to 20 cm of old soft snow. There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects and pockets of unconsolidated snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Last night's 5-10cm of fresh snow covers the recent melt-freeze crust. Below treeline the snowpack is trending isothermal in the afternoons depending on the overnight freeze. Higher elevations maintains softer snow with on-going multiple melt-freeze cycles. On north facing alpine slopes up to 15cm of surface snow overlies previous old dry surfaces.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of new snow overnight, accompanied by mod/strong Southerly winds, will have formed thin storm slabs at Tree-line and Alpine elevations. This sits on a strong melt/freeze crust. Below the crust, the snowpack is isothermal in thin snowpack areas BTL. The mid and lower snowpack is strong at Tree-line and above where depths are over 2m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In most areas we are seeing a typical spring snowpack with crusts breaking down in the heat of the day. Steep north facing alpine terrain is still holding dry snow. The midpack is generally moist and well settled. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Light dusting of snow over a melt-freeze crust on all areas, except alpine and treeline north and east aspects where there's up to 20 cm of old soft snow. There is still concern for a buried facet layer in the upper 30 cm of the snowpack on alpine N aspects and pockets of unconsolidated snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 5cm recent snow at upper elevations. Melt-freeze crusts on all aspects up to 2000m and higher all other aspects. On North and East aspects in the alpine, up to 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places and a weak, faceted snowpack, remains a concern in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The snowpack is trending isothermal in the afternoons on all aspects up to 2100m including N aspects. This condition tapers off as you ascend. North aspects treeline and above is still a winter snowpack. No windslab exists treeline and below but expect to find it high alpine ridgetops on generally East aspects in isolated terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of recent snow accompanied by 25-40km/hr Southerly winds formed wind slabs at Tree-line and Alpine elevations. The recent snow buries a melt freeze crust on all aspects to tree line. Below the crust, the snowpack is isothermal in thin snowpack areas BTL. The mid and lower snowpack is strong at Tree-line and above where depths are over 2m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 5cm recent snow at upper elevations. Melt-freeze crusts on all aspects up to 2000m and higher all other aspects. On North and East aspects in the alpine, up to 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places and a weak, faceted snowpack, remains a concern in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15cm recent snow at upper elevations. Melt-freeze crusts are common. On North and East aspects in the alpine, up to 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places and a weak, faceted snowpack, remains a concern in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Regular small snowfalls are settling quickly, over a melt-freeze crust everywhere except N aspects above treeline. Small windslabs are building on lee slopes (alpine and treeline). It's still a winter snowpack on alpine North aspects, with facets still producing sudden test results down 50cm, and whumphing in the South of the bulletin region. </span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15cm of recent snow with moderate Southerly winds has formed wind slabs at TL and ALP elevations. The recent snow buries a melt freeze crust on all aspects to tree line. Below the crust, the top 50cm is becoming moist during the day, isothermal in thin snowpack areas BTL. Elsewhere the lower snowpack is strong where over 2m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15cm recent snow at upper elevations. Melt-freeze crusts are common. On North and East aspects in the alpine, up to 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places and a weak, faceted snowpack, remains a concern in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15cm recent snow at upper elevations. Melt-freeze crusts are common. On North and East aspects in the alpine, up to 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places and a weak, faceted snowpack, remains a concern in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Recent small snowfalls are settling quickly, over a melt-freeze crust everywhere except N aspects above treeline. Small windslabs can be found on lee slopes (alpine and treeline). It's still a winter snowpack on high North aspects, with facets in isolated areas giving sudden test results down 50cm, and whumphing in the South of the region. </span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Pockets of wind slabs at tree line and alpine elevations. The 15cm of recent snow buries a melt freeze crust on all aspects to tree line. Below the crust, the top 50cm is becoming moist during the day, isothermal in thin snowpack areas BTL. Elsewhere the lower snowpack is strong where over 2m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15cm recent snow at upper elevations. Melt-freeze crusts are common. On North and East aspects in the alpine, up to 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places and a weak, faceted snowpack, remains a concern in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of snow from the weekend has accumulated above treeline. Crust are present on most aspects and elevations excluding high North. On high North, 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places. If any notable rain occurs, expect a loose wet problem to develop.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Recent small snowfalls are settling quickly, over a melt-freeze crust that extends in to the alpine on all apsects. Small windslabs can be found on lee slopes. A winter snowpack remains on alpine N aspects, with facets under an 20-50cm slab in isolated areas in the Icefields area and further South, and basal depth hoar in shallow snowpack areas. </span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Pockets of wind slabs at tree line and alpine elevations. The 15cm of recent snow buries a melt freeze crust on all aspects to tree line. Below the crust, the top 50cm is becoming moist during the day, isothermal in thin snowpack areas BTL. Elsewhere the lower snowpack is strong where over 2m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In most areas we are seeing a typical spring snowpack with crusts breaking down in the heat of the day. If you can get above snowline, expect to see 10-15cm of new, wet snow by Wednesday evening . The midpack is generally moist and well settled. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of snow from the weekend has accumulated above treeline. Crust are present on most aspects and elevations excluding high North. On high North, 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places. If any notable rain occurs, expect a loose wet problem to develop.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of snow from the weekend has accumulated above treeline. Crust are present on most aspects and elevations excluding high North. On high North, 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places. If any notable rain occurs, expect a loose wet problem to develop.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Incoming new snow will be covering a strong surface crust on all aspects below treeline, and in to the alpine on solar aspects. </span></p><p class="p_CC664AAA"><span class="s_1681A555">A winter snowpack remains on N aspects treeline and above, with small pockets of windslab in lees, facets under an 20-50cm slab in isolated areas, and a weak base of facets and depth hoar in shallow snowpack areas. </span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Pockets of wind slabs at tree line and alpine elevations. The 20cm of recent snow buries a melt freeze crust on all aspects to tree line. Below the crust, the top 50cm is becoming moist during the day, isothermal in thin snowpack areas BTL. Elsewhere the lower snowpack is strong where over 2m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of snow from the weekend has accumulated above treeline. Crust are present on most aspects and elevations excluding high North. On high North, 30cm of unconsolidated snow can be found. Below this, a stiff slab overlying weak facets remains a concern in some places. If any notable rain occurs, expect a loose wet problem to develop.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow by Wed morning has melted at low elevations and made for about 30 cm of dry powder on high elevation north aspects. This snow is well settled and bonded to the underlying layers. Surface crusts exists on most aspects and elevations in the morning, deteriorating by noon. Facets exist in the upper snowpack on high north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A supportive crust  exists to 2,100m near treeline. Higher up, at treeline and above, a winter snowpack remains on N aspects . Solar facing slopes have crusts extending higher into the alpine. At upper elevation a weak faceted layer buried down 20-50cm remains of concern. The snowpack sits on a weak base of facets and depth hoar.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reactive wind slabs overlie a well settled mid and lower snowpack in the alpine on polar aspects. A weak melt freeze crust is capping isothermal snow on all aspects to tree line; surface crusts will exist at higher elevations on solar aspects. Recent storm snow has been shedding easily over the past few days as loose and slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow by Wed morning has melted at low elevations and made for about 30 cm of dry powder on high elevation north aspects. This snow is well settled and bonded to the underlying layers. Surface crusts exists on most aspects and elevations in the morning, deteriorating by noon. Facets exist in the upper snowpack on high north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Melt-freeze with some good powder on dark, high aspects. Otherwise, surface crusts exist on most aspects and elevations in the morning, deteriorating by noon. Deep facets can be found on high north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A supportive crust exists to 2,100m near treeline. Higher up, at treeline and above, a winter snowpack remains on N aspects . Solar facing slopes have crusts extending higher into the alpine. At upper elevation a weak faceted layer buried down 20-50cm remains of concern. The snowpack sits on a weak base of facets and depth hoar.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the alpine, Isolated persistent slabs overlie surface hoar on shaded aspects, and melt-freeze crusts on solar aspects; beneath is a well settled mid and lower snowpack. A weak melt freeze crust is capping isothermal snow on all aspects to tree line; surface crusts exist at higher elevations on solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In most areas we are seeing a typical spring snowpack with crusts breaking down in the heat of the day. If you can get above snowline, expect to see 5cm of new, wet snow on Friday and 10cm on Saturday falling as rain at lower elevations. The midpack is generally moist and well settled. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Melt-freeze with some good powder on dark, high aspects. Otherwise, surface crusts exist on most aspects and elevations in the morning, deteriorating by noon. Deep facets can be found on high north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 to 30cm has fallen since April 9 with light winds. Freezing levels reach roughly 2200m each day and modest solar inputs have created new crusts. Facets 50 to 70cm deep remain a concern on alpine North aspects. Shallow areas in the alpine are also of concern often displaying no consolidated mid-pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Forecast winds and snow could create windslabs in the alpine. A supportive crust exists to 2,100m on all aspects and extends into the alpine on solar slopes. A winter snowpack remains on N aspects above treeline. At upper elevations a weak faceted layer down 20-50cm remains a concern. The snowpack sits on a weak base of facets and depth hoar.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the alpine, Isolated persistent slabs overlie surface hoar on shaded aspects, and melt-freeze crusts on solar aspects; beneath is a well settled mid and lower snowpack. A melt freeze crust is capping isothermal snow on all aspects to tree line; surface crusts exist at higher elevations on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 to 30cm has fallen since April 9 with light winds. Freezing levels reach roughly 2200m each day and modest solar inputs have created new crusts. Facets 50 to 70cm deep remain a concern on alpine North aspects. Shallow areas in the alpine are also of concern often displaying no consolidated mid-pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 to 30cm has fallen since April 9. the new snow is being pushed into small windslabs on lee N and E aspects. Facets 50 to 70cm deep produce clean, hard shears but have not produced an avalanche for a long time. Shallow bottomless facets can be found on high north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Forecast winds and snow could create windslabs in the alpine. A supportive crust exists to 2,100m on all aspects and extends into the alpine on solar slopes. A winter snowpack remains on N aspects above treeline. At upper elevations a weak faceted layer down 20-50cm remains a concern. The snowpack sits on a weak base of facets and depth hoar.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Last week's storm snow has formed pockets of windslab lee slope alpine and treeline locations. Expect a melt freeze crust on true solar aspects at treeline and alpine locations. Protected high north aspects are the best bet for late season powder. Below treeline a melt freeze crust covers isothermal snow on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 to 30cm has fallen since April 9. the new snow is being pushed into small windslabs on lee N and E aspects. Facets 50 to 70cm deep produce clean, hard shears but have not produced an avalanche for a long time. Shallow bottomless facets can be found on high north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 50cm has fallen at higher elevations since April 9. The new snow and wind is creating windslabs on lee N and E aspects, some up to 100cm deep in immediate lees in the alpine. Facets 50 to 70cm deep produce hard shears but have not produced an avalanche for a while. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Light snowfall and moderate SW wind building pockets of slab in the alpine. A supportive crust exists to 2,100m on all aspects and extends into the alpine on solar slopes. A winter snowpack remains on N alpine aspects, with a weak faceted layer down 20-50cm remaining a concern, and a facetted mid/lower snowpack that is weak in shallow areas.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm+ of storm snow overnight with mod to strong SW-S winds will be forming soft storm slabs on alpine and treeline lee slopes. Melt freeze crusts on steeper solar aspects and all aspects below treeline. The BTL crust may be weakened from being insulated by storm snow. Below treeline a melt freeze crust covers isothermal snow on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 50cm has fallen at higher elevations since April 9. The new snow and wind is creating windslabs on lee N and E aspects, some up to 100cm deep in immediate lees in the alpine. Facets 50 to 70cm deep produce hard shears but have not produced an avalanche for a while. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50cm has fallen at higher elevations since April 9. Recent winds and snow have created windslabs on lee N and E aspects in the alpine, up to 100cm deep. Still some uncertainty with the March 7 layer, snowpack structure and recent test show a weakness 50 to100cm down on high north aspects but no avalanche activity has been recently reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Above treeline 10cm of loose snow sits on a variety of crusts. Above 2200m, on Northerly facing slopes, a more winter like snowpack can be found. However, at and below 2200 melt-freeze crust dominate the upper snowpack. In the alpine a weak layer down 20-50cm is of concern. Mid and lower snowpack is faceted, and weak in shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm+ of storm snow in the last 48 hours with mod SW-S winds has formed storm slabs in the alpine and exposed areas of treeline. Storm slabs are overlying melt-freeze crust on all asp, and elev, except Nth alpine. Poor crust recovery BTL with the new snow insulating the melt freeze crust, which covers isothermal snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In most areas we are seeing a typical spring snowpack with crusts breaking down in the heat of the day. The exception is high North facing terrain where temperatures have stayed cold and a winter snowpack remains, with facets continuing to linger at the base. The midpack is generally well settled. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 50cm has fallen at higher elevations since April 9. Recent winds and snow have created windslabs on lee N and E aspects in the alpine, up to 100cm deep. Still some uncertainty with the March 7 layer, snowpack structure and recent test show a weakness 50 to100cm down on high north aspects but no avalanche activity has been recently reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Faceting continues. Snow surface conditions range from hard slabs to re-crystalized soft snow with little wind effect.&nbsp; The Nov 8 crust is down 20-30cm up to 2400m which is facetting over time. The lower snowpack is a mix of weak facets &amp; crusts. Snowpack depths at treeline vary from 60-90 cm with up to 140 cm in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The shallow snowpack areas will be faceting and loosing support underfoot though much of the forecast region due to the sustained cold temps. Windslabs and wind effect in exposed areas. The fervent hunter may find up to 10-20cm of soft snow found in sheltered S and W pitches. This sits over the Nov crust and is supportive to skis on solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temps are facetting the upper snowpack. Previous strong N'ly winds have redistributed last weekend's storm snow- watch for reverse loading. The main layer to watch (Nov 23rd surface hoar/ crust) is buried 25-45cm. This layer exists as a crust on all aspects below 1600m and on steep solar aspects into the alpine; surface hoar around treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A strong, localized wind event has scoured the majority of our terrain. Areas that still hold snow will have pockets of windslab and heavy loading.  New windslab overlies a variety of bed surface including bare ground, old windslab and a melt freeze crust where snow from the late Sept. snowfall did not melt out. Snowpack depth varies from 0 -90 cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Faceting continues. Snow surface conditions range from hard slabs to re-crystalized soft snow with little wind effect. The Nov 8 crust is down 20-30cm up to 2400m which is facetting over time. The lower snowpack is a mix of weak facets &amp; crusts. Snowpack depths at treeline vary from 60-90 cm with up to 140 cm in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Snow surface conditions range from hard slabs to re-crystalized soft snow with little wind effect. The Nov 8 crust is down 20-30cm up to 2400m which is facetting over time. The lower snowpack is a mix of weak facets &amp; crusts. Snowpack depths at treeline vary from 60-90 cm with up to 140 cm in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">The shallow snowpack areas will be faceting and loosing support underfoot though much of the forecast region due to the sustained cold temps. Windslabs and wind effect in exposed areas. Oct. and Nov. crusts preserved in the mid and lower snowpack; both seem have a good bond to the overlaying snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">8cm of snow overnight covers a facetted upper snowpack and previously wind affected surfaces. The main layer to watch (Nov 23rd surface hoar/ crust) is buried 25-45cm. This layer exists as a crust on all aspects below 1600m and on steep solar aspects into the alpine; surface hoar around treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Snow surface conditions range from hard slabs to re-crystalized soft snow with little wind effect. The Nov 8 crust is down 20-30cm up to 2400m which is facetting over time. The lower snowpack is a mix of weak facets &amp; crusts. Snowpack depths at treeline vary from 60-90 cm with up to 140 cm in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of fresh snow (and more expected on Wednesday) accompanied by moderate SW winds have created fresh windslabs in lee alpine terrain. The midpack consists of 25-35 cm of facetted snow overtop of the Nov 8 crust. The lower snowpack consists of facets and depth hoar. Snowpack depths at treeline vary from 60-90 cm with up to 140 cm in lee areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">New snow falling on to a mix of surfaces; surface facets, surface hoar, and previous windslab and/or hard wind pressed surfaces. New building windslabs in exposed areas in the alpine and treeline. Oct. and Nov. crusts preserved in the mid and lower snowpack; both seem have a good bond to the overlaying snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> 30 of new snow covers a facetted upper snowpack and previously wind affected surfaces. The two main interfaces to watch for are the storm slab interface down 30cm+ and the Nov 23rd surface hoar/ crust buried 40-60cm. Multiple buried crusts exist lower in the snowpack, but recent profiles are showing no significant shears on stability tests.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of fresh snow (and more expected on Wednesday) accompanied by moderate SW winds have created fresh windslabs in lee alpine terrain. The midpack consists of 25-35 cm of facetted snow overtop of the Nov 8 crust. The lower snowpack consists of facets and depth hoar. Snowpack depths at treeline vary from 60-90 cm with up to 140 cm in lee areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 30cm of new snow accompanied by moderate to strong SW winds have created fresh wind slabs on lees slopes at treeline and above. The midpack consists of 25-35 cm of facetted snow overtop of the Nov 8 crust. The lower snowpack consists of facets and depth hoar. Snowpack depths at treeline vary from 60-100 cm with up to 140 cm in lee areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Up to 30cm of new snow in the Columbia Icefields area fell on to a mix of surfaces; surface facets, surface hoar, and previous wind slab and/or hard wind pressed surfaces. The moderate winds built soft wind slabs at ridge tops. Oct. and Nov. crusts are preserved in the mid and lower snowpack and both seem have a good bond to the overlaying snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Approximately 60-70cm of storm snow overlies a variety of facetted surfaces, crusts or old wind slabs depending on aspect and elevation. The two main interfaces to watch for are the storm slab interface and the Nov 23rd surface hoar/ crust buried 40-60cm. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 30cm of new snow accompanied by moderate to strong SW winds have created fresh wind slabs on lees slopes at treeline and above. The midpack consists of 25-35 cm of facetted snow overtop of the Nov 8 crust. The lower snowpack consists of facets and depth hoar. Snowpack depths at treeline vary from 60-100 cm with up to 140 cm in lee areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 30cm of new snow accompanied by moderate to strong SW winds have created fresh wind slabs on lees slopes at treeline and above. The midpack consists of 25-35 cm of facetted snow overtop of the Nov 8 crust. The lower snowpack consists of facets and depth hoar. Snowpack depths at treeline vary from 60-100 cm with up to 140 cm in lee areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Up to 30cm of new snow in the Columbia Icefields area fell on to a mix of surfaces; surface facets, surface hoar, and previous wind slab and/or hard wind pressed surfaces. The moderate winds built soft wind slabs at ridge tops. Oct. and Nov. crusts are preserved in the mid and lower snowpack and both seem have a good bond to the overlaying snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Approximately 70cm of snow has fallen since December 2. The new snow is poorly bonded to buried layers. During the peak of the storm, strong winds formed touchy slabs on lee features in the alpine. The November 23rd surface hoar/crust layer is buried 60-80cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent Warm temperatures have created a weak melt freeze crust on all aspects up to 2200m. Areas that still hold snow will have windslab overlying a variety of bed surface including bare ground, and a melt freeze crust where snow from the late Sept. snowfall did not melt out. Snowpack depth varies from 0 -70cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 to 30cm of new snow accompanied by moderate to strong SW winds have created fresh wind slabs on lees slopes at treeline and above. The midpack consists of 25-35 cm of facetted snow overtop of the Nov 8 crust. The lower snowpack consists of facets and depth hoar. Snowpack depths at treeline vary from 60-100 cm with up to 140 cm in lee areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40-50cm of new snow has fallen with moderate to strong SW winds, a storm slab is building in the Alpine down to Treeline. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is up to 2400m and ~30cm up from ground. Snowpack depths at treeline are 80-130cm and deeper in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Up to 40cm of recent snow in the Columbia Icefields area fell on to a mix of surfaces; surface facets, surface hoar, and previous wind slab and/or hard wind pressed surfaces. The moderate winds built soft wind slabs at ridge tops. Oct. and Nov. crusts are preserved in the mid and lower snowpack are breaking down with faceting.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 cm of low density snow fell overnight and sits atop 70cm of settling storm snow. Winds from the previous storm created slabs on lee alpine features which are now concealed by the new snow. The November 23rd surface hoar/crust layer is buried +100cm and remains reactive in stability tests. Tree wells are getting deeper and deserve extra caution. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40-50cm of new snow has fallen with moderate to strong SW winds, a storm slab is building in the Alpine down to Treeline. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is up to 2400m and ~30cm up from ground. Snowpack depths at treeline are 80-130cm and deeper in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50+ cm of snow has fallen since Tuesday with moderate to strong SW winds. A storm slab has formed at treeline and above. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust exists up to 2400m and 30 cm up from ground. Snowpack depths at treeline are 80-130 cm and deeper in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">40 to 50 cm of snow has fallen since Tuesday on a mix of surfaces; ground, surface facets, surface hoar, and previous wind slab and/or hard wind pressed surfaces. Moderate SW winds are building soft wind slabs at ridge tops. The Oct. and Nov. crusts are present in the mid and lower snowpack. Basal facets are weak and are changing into depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of snowfall in the last 30hrs rests on top of 70cm of settling storm snow from this past week. The previous storm created slabs on lee alpine features which are now concealed. The November 23rd surface hoar/crust layer is buried +100cm and remains reactive in stability tests. Tree wells are deep and deserve extra caution, buddy up.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50+ cm of snow has fallen since Tuesday with moderate to strong SW winds. A storm slab has formed at treeline and above. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust exists up to 2400m and ~30cm up from ground. Snowpack depths at treeline are 80-150+cm and deeper in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40-60+ cm of snow has fallen in the last 4 days. A storm slab has formed at treeline and above. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust exists up to 2500m and 30 cm up from ground. Snowpack depths at treeline are 80-130 cm and deeper in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow continues to settle but the cold temps are slowing any formation of a surface slab except for specific southerly locations at or below tree line. The snow depths are variable and the recent storm snow overlies a variety of layers depending on aspect, elevation and shelter from the wind. Wind slabs continue to form.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40cm of recent storm snow (since Dec. 5th), overlies surface hoar up in sheltered locations, and is concealing evidence of the recent cycles of large to very large natural avalanches. The November 23rd surface hoar/crust/facet layer is buried 80-100+cm and remains reactive in stability tests. Tree wells are deep and deserve extra caution.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm low density storm snow coupled with moderate west winds has formed new slabs in the alpine and treeline. This overlies previous windslabs and a crust below 2200m. A melt freeze crust complex formed throughout October and November forms the base of the snowpack, and this will be a layer to keep an eye on as the season continues.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40-60+ cm of snow has fallen in the last 4 days. A storm slab has formed at treeline and above. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust exists up to 2500m and 30 cm up from ground. Snowpack depths at treeline are 80-130 cm and deeper in lee areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate winds in the alpine creating small wind slabs. Recent storm snow has formed a slab at treeline and above. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow is mostly unconsolidated except where exposed to wind where soft slabs have been formed.  The snow depth is variable at all elevations.  There is a reactive crust in the mid-pack and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate S-SW winds building fresh wind slabs in the alpine. 40cm of previous storm snow (since Dec. 5th) overlies surface hoar in some locations TL and BTL, and is concealing evidence of the recent cycle of natural avalanches. The November 23rd surface hoar/crust/facet layer is buried 80-100+cm and remains reactive in stability tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm storm snow coupled with moderate west winds has formed new slabs in the alpine. This overlies previous windslabs and a crust below 1800m. A melt freeze crust facet combo formed at the start of the season sits at the bottom of the snowpack. Though unlikely to be triggered by people, we have seen other avalanches stepping down to this layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate winds in the alpine creating small wind slabs. Recent storm snow has formed a slab at treeline and above. Below the storm slab, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate winds in the alpine are adding to the wind slabs problem in the alpine. Beneath the recent 40-60 cm of recent snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent snow remains unconsolidated except where exposed to wind and soft slabs have been formed. The snow depth is variable at all elevations. There is a crust/facet layer distributed through the region in the mid-pack with mixed reactivity and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate S-SW winds have created wind slabs in lee alpine features. 40cm of storm snow (since Dec. 5th) overlies surface hoar in some locations TL and BTL, and is concealing evidence of the recent cycle of natural avalanches. The November 23rd surface hoar/crust/facet layer is buried 80-100+cm and remains reactive in stability tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate winds in the alpine are adding to the wind slabs problem in the alpine. Beneath the recent 40-60 cm of recent snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate winds in the alpine are adding to the wind slabs problem. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The top 30cm remains unconsolidated except where exposed to wind where soft slabs have been formed. The snow depth is variable at all elevations. There is a crust/facet layer distributed through the region in the mid-pack with mixed reactivity and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate S-SW winds have created wind slabs in lee alpine features. Clear skies and cool temps have promoted faceting in the new snow, as well as surface hoar growth. The Dec 5 surface hoar is 30-40cm down and is stubborn in tests. The November 23rd surface hoar/crust/facet layer is buried 80-100+cm and is becoming stubborn in stability tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snow amount vary through the forecast region. Areas north of the HWY1 (little Yoho) received 50-70cm last week creating a well developed early winter snowpack. These typical deeper snowpack areas have few faceted layers and are begging to form a settled mid pack. Around Field the snowpack is much shallower resembling the Banff forecast region. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong winds in the alpine have increased wind slab thickness. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The top 30cm remains unconsolidated except where exposed to wind where soft slabs have been formed. The snow depth is variable at all elevations. There is a crust/facet layer distributed through the region in the mid-pack with mixed reactivity and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Light snowfall has now buried the Dec 11 surface hoar layer. S-SW winds have recently formed windslab on ALP lee slopes. Cold temps and clear skies have faceted the recent snow surface. The Dec 5th surface hoar is down +/-40cm and is stubborn in tests. The Nov 23rd surface hoar/crust/facet combo is down +/-100cm and is becoming stubborn in tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm previous storm snow coupled with strong to extreme west winds has formed new slabs in the alpine and treeline. A melt freeze crust facet combo formed at the start of the season sits at the bottom of the snowpack. Though unlikely to be triggered by people, it is not impossible and we have seen other avalanches stepping down to this layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong winds in the alpine have increased wind slab thickness. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak with facets and depth hoar where under 1 meter. The exception to this so far has been the Takakkaw falls area which has a much deeper and stronger snowpack at  treeline and below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable wind slabs from the past 2 days have formed mainly in the alpine. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The top 30cm remains unconsolidated except where exposed to wind where soft slabs have been formed. The snow depth is variable at all elevations. There is a crust/facet layer distributed through the region in the mid-pack with mixed reactivity and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm snow now buries the Dec 11 surface hoar layer. S-SW winds have recently formed windslab on ALP lee slopes. Earlier cold temps and clear skies faceted the past snow surface. The Dec 5th surface hoar is down +/-40cm and is stubborn in tests. The Nov 23rd surface hoar/crust/facet combo is down +/-100cm and is becoming more stubborn in tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has been variable wind slab development mainly in the alpine over the last two days. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak with facets and depth hoar where under 1 meter. The exception so far has been the Takakkaw falls area which has a much deeper and stronger snowpack at treeline and below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Pockets of wind slab linger in alpine areas. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The top 30cm remains unconsolidated except where exposed to wind where soft slabs have been formed. The snow depth is variable at all elevations. There is a crust/facet layer distributed through the region in the mid-pack with mixed reactivity and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15cm of new snow now buries the Dec 11 surface hoar layer. This new snow, combined with light southerly wind, is building pockets of soft storm slab in the Alpine. The Nov 23rd surface hoar/crust/facet combo is down +/-100cm and is becoming more stubborn in tests, but continues to show it's potential to propagate well once triggered.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Pockets of wind slab linger in alpine areas. Beneath the recent 40-60cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. In areas with a deeper snowpack (Tak Falls, Stanley Mitchell, Ogden, etc.) the basal weakness is less pronounced.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Pockets of wind slab linger in alpine areas. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The top 30cm remains unconsolidated except where exposed to wind and soft slabs may have been formed. The snow depth is variable at all elevations. There is a crust/facet layer distributed through the region in the mid-pack with mixed reactivity and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20 cm of new snow now buries the Dec 11 surface hoar layer. This new snow, combined with light southerly wind, is building pockets of soft storm slab in the Alpine. The Nov 23rd surface hoar/crust/facet combo can be found down +/-100cm (SH is most prevalent in sheltered treeline locations) but has become increasingly stubborn in testing.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Pockets of wind slab linger in alpine areas. Beneath the recent 40-60cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. In areas with a deeper snowpack (Tak Falls, Stanley Mitchell, Ogden, etc.) the basal weakness is less pronounced.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reactive, thin (~10cm) new windslabs are being created by increased west wind. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Top 30cm of the snowpack is mostly unconsolidated except where exposed to wind and slabs may have been formed. The snow depth is variable at all elevations. There is a crust/facet layer distributed through the region in the mid-pack with mixed reactivity and a weak basal facet/depth hoar layer at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20+ cm of new snow now buries the Dec 11 surface hoar layer. Moderate S'ly winds are building pockets of soft storm slab in the Alpine. The Nov 23rd surface hoar/crust/facet combo is down +/-100cm (SH is most prevalent in sheltered treeline locations) but has become increasingly stubborn in testing. The mid-lower snowpack is settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A true rockies snowpack! Windslabs exist at all elevations, especially in burnt areas. A problematic weak crust facet combo formed in November is down 60cm, and additional crust/facet layers formed in October form the bottom of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New windslabs are being created by increased west wind. Beneath the recent 40-60cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. In areas with a deeper snowpack (Tak Falls, Stanley Mitchell, etc.) the basal weakness is less pronounced.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong winds have formed new wind slab at alpine and tree line. The distribution of this new load is uncertain. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate SW winds and high relative humidity firming up the top 30cm creating soft and hard slabs. The snow depth is variable at all elevations. There is a mid-pack crust/facet layer distributed through the region. It has mixed reactivity. A weak basal facet/depth hoar layer exists at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40cm of new snow now buries the Dec 11 surface hoar layer. Moderate S'ly winds are building storm slabs in the Alpine. The Nov 23rd surface hoar/crust/facet combo is down +/-100cm (SH is most prevalent in sheltered treeline locations) but has become increasingly stubborn in testing. The mid-lower snowpack is settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New wind slab can be found on immediate lees alpine and tree line, the extent of the distribution is uncertain. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong winds have formed new wind slabs at alpine and tree line. The distribution of this new load is uncertain. Beneath the recent 40-60 cm of storm snow, the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sustained moderate to strong SW ridge-top winds likely creating variable soft and hard slabs in all lee features. There is a mid-pack crust/facet interface distributed through the region. It has shown very little reactivity to this point. A weak basal facet/depth hoar layer exists at the base of the pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50-60cm of new snow now buries the Dec 11 surface hoar layer. New snow, Moderate winds built storm slabs at all elevations. The Nov 23rd surface hoar/crust/facet combo is down +/-100cm (SH is most prevalent in sheltered treeline locations) but has become increasingly stubborn in testing. The mid-lower snowpack is settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong winds have formed new wind slabs at alpine and tree line. In thin snowpack areas (Mt. Dennis), the snowpack consists of recent storm snow over a weak base of facets and depth hoar. In thicker areas (140 cm +) the snowpack is more settled and less faceted. The Nov Crust is present upto 2500 m and ~30 cm up from ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent strong winds have formed wind slabs in the alpine and exposed tree line areas. The snowpack structure is generally weak, consisting of facets and depth hoar and will be stressed by the incoming storm snow. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong SW ridge winds continue building varied strength windslabs on lee and crossloaded features at or above treeline. Persistent interfaces layered through the snowpack that might wake as the up to as the 25cm's of new snow forecasted in the next 24 hours accumulates.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">60-70cm of new snow now buries the Dec 11 surface hoar layer. Previous new snow, and moderate winds built storm slabs at all elevations. The Nov 23rd surface hoar/crust/facet combo is down +/-120cm but has become increasingly stubborn in testing. Both of these interfaces are expected to wake up this weekend!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow will be falling on variable wind affected surfaces from extreme west winds. A weak crust facet combo formed in November is down 60cm, and additional crust/facet layers formed in October form the bottom of the snowpack. These are less of a problem in deeper snowpack areas along the divide, but may be overloaded with incoming snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent strong winds have formed wind slabs in the alpine and exposed tree line areas. The snowpack structure is generally weak, consisting of facets and depth hoar and will be stressed by the incoming storm snow. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-35cm of storm snow in the past 24hrs accompanied by moderate Southerly winds is forming a storm slab in the alpine and at tree line. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 90-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm new over the last 6 hours, Light winds continue building variable strength wind slabs on lee and crossloaded features at or above treeline. Persistent interfaces layered through the snowpack that might wake as the up to as the 35cm's of new snow forecasted in the next 36 hours accumulates.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Field tests and observations found a reactive storm slab down 20cm. 80cm+ of snow now buries the Dec 11 surface hoar layer. Previous new snow, and mod winds built storm slabs at all elevations. The Nov 23rd surface hoar/crust/facet combo is down +/-130cm has become increasingly stubborn in testing. These interfaces are expected to wake up today.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of wet snow and rain has arrived with extreme northwest winds and a freezing level around 1900m, providing a shock to the snowpack. A weak crust facet combo formed in November is down 60cm, and additional crust/facet layers formed in October form the bottom of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-35cm of storm snow in the past 24hrs accompanied by moderate Southerly winds is forming a storm slab in the alpine and at tree line. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar. The Nov crust is present up to 2500m and ~30 cm up from ground. Snowpack depths at treeline range from 90-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-70cm of warm, wet snow in the past 48hrs with moderate to strong S/SW winds.  Storm slabs have formed at all elevations and aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m.  These weak layers are getting overloaded with all of the new snow.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 100cm new snow in the last 48 hours with very little wind effect. This overlies wind slab and a variety of weak layers near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">60cm of storm snow now sits on 70cm of recent snow, which overlies the Dec 11th SH (5-12mm). This sits on a rounding midpack. The Nov 23 SH/Cr is down 160-185cm. Early season crusts still persist in the lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">60cm+ of wet snow and rain in the Cameron Lake area has arrived with extreme northwest winds and a freezing level around 1900m, continuing to load the snowpack. A weak crust facet combo formed in November is down 60cm, and additional crust/facet layers formed in October form the bottom of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-70cm of warm, wet snow in the past 48hrs with moderate to strong S/SW winds. Storm slabs have formed at all elevations and aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow since Friday has formed storm slabs all elevations and aspects. At upper elevations evidence new wind transport is visible. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow fallen in the last 48 hours with very little wind effect and variable slab cohesion. This overlies wind slab and a variety of weak layers near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The Atmospheric River dumped 75mm of precipitation since Thursday afternoon. The Dec 11th SH (5-12mm) is now down 90-120cm, and sits on a rounding midpack. The Nov 23 SH/Cr is down 160-185cm. Early season crusts still persist in the lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow since Friday has formed storm slabs all elevations and aspects. At upper elevations evidence new wind transport is visible. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow has formed storm slabs all elevations and aspects. At upper elevations evidence new wind transport is visible. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">45cms of mostly undisturbed HST continues to settle and with cold temperatures tighten up. This overlies a mosaic of buried wind slab, ground and facetted weak layers. Basal layers continue to develop into larger facets and depth hoar. Surface hoar continue to grow in sheltered areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The Atmospheric River dumped 75mm of precipitation over the weekend, and is settling slowly with cooling temperatures. The Dec 11th SH (5-12mm) is now down 90-120cm, and sits on a rounding midpack. The Nov 23 SH/Cr is down 160-185cm. Early season crusts still persist in the lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is a highly variable snowpack across the forecast region. Generally the snowpack is wet and thin below 1800m. Above that elevation, the Cameron Lake area received the most snow in the storm with 85-100cm since Thursday. This sits on a weak facet/crust combo that is now down 150cm. The front ranges hold a thinner more wind affected snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow has formed storm slabs all elevations and aspects. At upper elevations evidence new wind transport is visible. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow has formed storm slabs all elevations and aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">45cms of mostly undisturbed storm snow blanketing the region. This overlies a mosaic of buried wind slabs and facetted weak layers. Basal layers continue to develop into larger facets and depth hoar. Surface hoar growing in sheltered areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The top 70cm of snow remains fairly unconsolidated in most places, and still has that post-storm powdery feeling. A new surface crust exists on steep solar aspects. The Dec 11th SH (5-12mm) is well preserved and is now down 90-120cm. The Nov 23 SH/Cr is down 160-185cm. Early season crusts still persist in the lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is a highly variable snowpack across the forecast region. Generally the snowpack is wet and thin below 1800m capped by a met freeze crust. Above that, the Cameron Lake area received  85-100cm since Thursday. This sits on a weak facet/crust combo that is now down 150cm. The front ranges hold a thinner more wind affected snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow has formed storm slabs all elevations and aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow has formed storm slabs all elevations and aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">45cms of mostly undisturbed storm snow blanketing the region. This overlies a mosaic of buried wind slabs and facetted weak layers. Basal layers continue to develop into larger facets and depth hoar. Surface hoar growing in sheltered areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The top 50cm is forming into soft slabs especially near ridge crests. A new surface crust exists on steep solar aspects. The Dec 11th SH (5-12mm) is well preserved and is now down 90-120cm. The Nov 23 SH/Cr is down 160-185cm. Early season crusts still persist in the lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm of settled storm snow has formed storm slabs all elevations and aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface hoar growth up to 5mm observed below tree line. Moderate SW winds are redistributing the 30-60cm of recent storm snow and forming wind slab on lee aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">6-20mm Surface Hoar growing up to 2200m. 45cms of mostly undisturbed storm snow blanketing the region. This overlies a mosaic of buried wind slabs and facetted weak layers. Basal layers continue to develop into larger facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Last week's metre of snow is settling into a soft slab, especially near ridge crests. A thin sun crust exists on steep solar aspects. The Dec 11th SH (5-12mm) is well preserved and is now down 90-120cm. Early season crusts still persist in the lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface hoar growth up to 5mm observed below tree line. Moderate SW winds are redistributing the 30-60cm of recent storm snow and forming wind slab on lee aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface hoar growth up to 5mm observed below tree line. Moderate SW winds are redistributing the 30-60cm of recent storm snow and forming wind slab on lee aspects. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">6-20mm Surface Hoar growing up to 2200m. Consistent Moderate SW winds for the past 36 hours have created wind slabs in lee features. This overlies a mosaic of buried wind slabs and facetted weak layers. Basal layers continue to develop into larger facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm HN24 fell on top of yesterdays SH and the 80 to 120cm that is now over the Dec 11th SH (5-12mm). Slabs have formed in the lees of ridge crests and a thin crust on steep solar aspects is now under the new snow. Early season crusts still persist in the lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is thin below 1800m and capped by a met freeze crust. Above 1800m, 85-120cm of snow from last weeks storm sits on top of a weak facet/crust combo. The front ranges hold a thinner, more wind affected, snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface hoar growth up to 5mm observed below tree line. Moderate SW winds are redistributing the 30-60cm of recent storm snow and forming wind slab on lee aspects. Below the new snow the snowpack structure is generally weak  consisting of facets and depth hoar and a Nov crust up to 2500m. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to Strong W and SW winds have redistributed snow in the alpine and the upper areas of treeline. Snowpack depths at treeline range from 100 to 160cm. The Nov crust is found ~ 30cm above the ground and is present up to 2500m. The weak facets sitting above this crust are an obvious weakness and are more developed in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">6-25mm Surface Hoar growing up to 2200m. Consistent Moderate SW winds for the past 48 hours have created wind slabs in lee features. These overlies a mosaic of buried wind slabs and facetted weak layers. Basal layers continue to develop into larger facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm new snow in 48hrs on top of surface hoar at treeline and a thin crust on steep solar aspects. The cold temperatures this week have weakened the top 50cm of previous storm snow. Below that it is quite stiff down to the Dec 11th surface hoar (5-12mm) which is now down 90-130cm. Early season crusts still persist in the rounding lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to Strong W and SW winds have redistributed snow in the alpine and the upper areas of treeline. Snowpack depths at treeline range from 100 to 160cm. The Nov crust is found ~ 30cm above the ground and is present up to 2500m. The weak facets sitting above this crust are an obvious weakness and are more developed in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong W and SW winds have redistributed snow in the alpine and the upper areas of treeline. Snowpack depths at treeline range from 100 to 160cm. The Nov crust is found ~ 30cm above the ground and is present up to 2500m. Weak facets below this depth are the obvious weakness and are more developed in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">6-25mm surface hoar growing up to 2200m in sheltered areas. SW winds have created wind slabs on lee features treeline and above. These surface windslabs sit on a variety of buried wind slabs and facetted weak layers. In sheltered areas, the snowpack is weak and faceted. The bottom of the snowpack is also weak with large facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm recent new snow on top of surface hoar at treeline and a thin crust on steep solar aspects. The cold temperatures this week have weakened the top 50cm of previous storm snow. Below that it is quite stiff down to the Dec 11th surface hoar (5-12mm) which is now down 90-130cm. Early season crusts still persist in the rounding lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong W and SW winds have redistributed snow in the alpine and the upper areas of treeline. Snowpack depths at treeline range from 100 to 160cm. The Nov crust is found ~ 30cm above the ground and is present up to 2500m. Weak facets below this depth are the obvious weakness and are more developed in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow and moderate to strong SW winds are creating new wind slabs in lee areas at and above treeline. In most areas the upper snowpack of denser snow sits over a weak mid and lower snowpack consisting of facets, depth hoar and crusts. In deeper snowpack areas these weaknesses are less pronounced. Snowpack depths at treeline average 100-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of settling snow sits on top of surface hoar and a thin crust on steep S aspects. Recent cold temps have facetted the upper snowpack, but have not penetrated into the stiff snow that overlies the Dec 11th surface hoar (5-12mm) which persists down 90-130cm. Several crusts exist in the rounding lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong Westerly winds continue to develop Windslab at treeline &amp; above. A deteriorating melt freeze crust exists on all aspects up to 1800m. Above 1800m, 85-120cm of well settled snow from last weeks storm sits on top of a weak facet/ melt freeze crust near the base of the snowpack. Reactivity of this basal weakness is variable &amp; warrants caution.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow and moderate to strong SW winds are creating new wind slabs in lee areas at and above treeline. In many areas the upper snowpack of denser snow sits over a weak mid and lower snowpack consisting of facets, depth hoar and crusts. In deeper snowpack areas these weaknesses are less pronounced. Snowpack depths at treeline average 100-160+ cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow and moderate SW winds are creating new wind slabs in lee areas at and above treeline. In most areas the upper snowpack of denser snow sits over a weak mid and lower snowpack consisting of facets, depth hoar and crusts. In deeper snowpack areas these weaknesses are less pronounced. Snowpack depths at treeline average 100-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Large surface hoar growing up to 2200m in sheltered areas. SW winds have created wind slabs on lee features treeline and above. These windslabs sit on a variety of buried wind slabs and facetted weak layers. The bottom of the snowpack consists of facets, decomposing crusts and pronounce depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-30cm of new snow fell since the 27th of Dec, burying a 5mm Surface Hoar layer. Mod to Strong S-SW winds yesterday pm redistributed the new snow on lee features in the Alpine and exposed areas of Tree Line. The mid and lower snowpack has been settling and gaining strength; however, the Dec 11th surface hoar (5-12mm) still persists down 90-130cm. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong - Extreme Westerly winds continue to develop Windslab in lee areas. A deteriorating melt freeze crust exists on all aspects up to 1800m. Above 1800m, 85-120cm of well settled snow from previous storm sits on top of a weak facet/ melt freeze crust near the base of the snowpack. Reactivity of this basal weakness is variable &amp; warrants caution.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow and moderate SW winds are creating new wind slabs in lee areas at and above treeline. In most areas the upper snowpack of denser snow sits over a weak mid and lower snowpack consisting of facets, depth hoar and crusts. In deeper snowpack areas these weaknesses are less pronounced. Snowpack depths at treeline average 100-160+ cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thin/soft windslabs forming on the surface near ridge top from light NW wind and 5-10 cm overnight. In most areas the upper snowpack of denser snow sits over a weak mid and lower snowpack consisting of facets, depth hoar and crusts. In deeper snowpack areas these weaknesses are less pronounced. Snowpack depths at treeline average 100-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable amounts of snowfall through the region, burying large surface hoar, present up to 2200m in sheltered areas. SW winds continue to created new wind slabs on lee features at treeline and above. The bottom of the snowpack consists of very pronounced facets, decomposing crusts and depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40-50cm of snow now sits on the Dec 27th surface hoar. Previous Mod to Strong S-SW winds redistributed the new snow on lee features in the Alpine and exposed areas of Tree Line. The mid and lower snowpack has been settling and gaining strength; however, the Dec 11th surface hoar (5-12mm) still persists down 100-140cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thin/soft windslabs forming on the surface near ridge top from light NW wind and 5-10 cm overnight. In most areas the upper snowpack of denser snow sits over a weak mid and lower snowpack consisting of facets, depth hoar and crusts. In deeper snowpack areas these weaknesses are less pronounced. Snowpack depths at treeline average 100-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15 cm over the past 2 days. The alpine has been hammered by W wind creating wind slabs in the alpine to treeline. Generally, the upper snowpack of denser snow sits over a weak lower snowpack consisting of facets, depth hoar and crusts. At treeline, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> An additional 9cm last night in the parkers area. Variable amounts of snowfall through the region, burying large surface hoar, present up to 2200m in sheltered areas. SW winds continue to created new wind slabs on lee features at treeline and above. The bottom of the snowpack consists of very pronounced facets, decomposing crusts and depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50-70cm of storm snow now sits on the Dec 27th surface hoar. Strong S-SW winds are redistributing the storm snow on lee features in the Alpine and exposed areas of Treeline. The mid and lower snowpack has been settling and gaining strength; however, the Dec 11th surface hoar (5-12mm) still persists down 120-160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At cameron Lake, a 20-60cm Windslab had developed over the past week. The Middle of the snowpack is well settled but a weak facet/ melt freeze crust still lurks near the base of the snowpack. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The Front ranges have a deteriorating melt freeze crust up to 1800m on top of a faceted lower snowpack. Shallow snowpack areas require extra caution.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15 cm over the past 2 days. The alpine has been hammered by W wind creating wind slabs in the alpine to treeline. Generally, the upper snowpack of denser snow sits over a weak lower snowpack consisting of facets, depth hoar and crusts. At treeline, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures is promoting storm slab formation. Generally, the upper snowpack of denser snow sits over a weak lower snowpack consisting of facets, depth hoar and crusts. At tree line, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 25cm HST has fallen in the past 36 hours with an additional 30cm forecasted for tonight and into tomorrow. Buried surface hoar, present up to 2200m in sheltered areas. SSW winds continue to created new wind slabs on lee features at treeline and above. The bottom of the snowpack consists of pronounced facets, decomposing crusts and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50-70cm of storm snow now sits on the Dec 27th surface hoar. Strong S-SW winds are redistributing the storm snow to alpine lees and in exposed areas at treeline. The mid and lower snowpack has been settling and gaining strength but the Dec 11th surface hoar (5-12mm) still persists down 120-160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures is promoting storm slab formation. Generally, the upper snowpack of denser snow sits over a weak lower snowpack consisting of facets, depth hoar and crusts. At tree line, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures is promoting storm slab formation. Generally, the upper snowpack of denser snow sits over a weaker lower snowpack consisting of facets, depth hoar and crusts. At tree line, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 50cm of snow has fallen in the past 72 hours. Buried surface hoar is present up to 2200m in sheltered areas. Moderate SSW winds continue to create wind slabs on lee features at treeline and above. The bottom of the snowpack consists of well developed facets, depth hoar, and decomposing crusts. The bottom is weak. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50-70cm of storm snow now sits on the Dec 27th surface hoar. Strong S-SW winds are redistributing the storm snow to alpine lees and in exposed areas at treeline. The mid and lower snowpack has been settling and gaining strength but the Dec 11th surface hoar (5-12mm) still persists down 120-160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures are promoting storm slab formation. Some of the region has a midpack which sits over facets and depth hoar at the base, and other deeper areas have a well settled snowpack with limited facets and weak layers.  Digging down to see what is in the snowpack in your area is important. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures is promoting storm and wind slab formation. At tree line, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects. Generally, the upper snowpack of denser snow sits over a weaker lower snowpack consisting of facets, depth hoar and crusts. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 35cm of settling new snow below treeline overlies buried surface hoar up to 2200m in sheltered areas. Moderate SW winds continue to create and build on existing wind slabs on lee features at treeline and above. The bottom of the snowpack consists of well developed facets, depth hoar, and decomposing crusts.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme South winds have build reactive slabs well down into the slope in lee terrain. Several weaknesses can be found within the 65-90cm of storm snow above the persistent Dec 27th layer. The mid and lower snowpack has been gaining strength, but a few deep avalanches recently indicate early season weaknesses may be getting overloaded.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures are promoting storm slab formation. Some of the region has a midpack which sits over facets and depth hoar at the base, and other deeper areas have a well settled snowpack with limited facets and weak layers. Digging down to see what is in the snowpack in your area is important. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures is promoting storm and wind slab formation. At tree line, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects. Generally, the upper snowpack of denser snow sits over a weaker lower snowpack consisting of facets, depth hoar and crusts. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of settling new snow below treeline overlies buried surface hoar up to 2200m in sheltered areas. Moderate SW winds continue to build on existing wind slabs on lee features at treeline and above. The bottom of the snowpack consists of well developed facets, depth hoar, and decomposing crusts.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme S winds may have built reactive slabs well down into the slope in lee terrain. Several weaknesses can be found within the 65-90cm of storm snow above the persistent Dec 27th layer. The mid and lower snowpack have been gaining strength, but a few deep avalanches recently indicate early season weaknesses may be getting overloaded.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent Strong to Extreme winds have stripped windward slopes creating windslabs in lee areas, under which a thick crust exists to 1800m. The Middle of the snowpack is well settled, but a weak facet/ melt freeze crust still lurks near the base of the snowpack. Cornices have grown large.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack in the front ranges is much thinner and weaker.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of storm snow, strong Westerly winds and mild temperatures are promoting slab formation. Most areas have generally supportive midpack over facets and depth hoar at the base. In deeper areas the snowpack is well settled with limited facets and weak layers. Digging down to see what is in the snowpack in your area is important. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of snow, and strong wind from last few days have formed wind and storm slabs. At tree line, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects. Generally, the upper snowpack of denser snow sits over a weaker lower snowpack consisting of facets, depth hoar and crusts. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of new snow forecasted could overlie last weeks storm snow. Possible wind slab formation could occur on lee aspects in the alpine and treeline. These would overlie buried surface hoar up to 2200m in sheltered areas. Wind slabs on lee features at treeline and above. The bottom of the snowpack consists of depth hoar and facets</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Rogers Pass has received 100mm of precip in the past week, accompanied by strong to extreme S winds. Several weaknesses can be found within the 65-90cm of snow that lays above the persistent Dec 27th layer. The mid and lower snowpack have been strengthening, but don't forget about early season weaknesses with the increased load today.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of snow, and strong wind from last few days have formed wind and storm slabs. Most areas have generally supportive midpack over facets and depth hoar at the base. In deeper areas the snowpack is well settled with limited facets and weak layers. Digging down to see what is in the snowpack in your area is important.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of snow, and strong wind from last few days have formed fresh wind and storm slabs. At tree line, new snow sits on pockets of surface hoar in sheltered areas and sun crust on steep solar aspects. Generally, a settled mid-pack sits over a weaker lower snowpack consisting of facets, depth hoar and crusts. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A total of 65cm of storm snow since January 1st. Wind effect and slab formation on lee aspects in the alpine and treeline. This overlies buried surface hoar up to 2200m in sheltered areas as well as buried wind slabs on lee features at treeline and above. Well consolidated midpack. The bottom of the snowpack consists of depth hoar and facets</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Whoa! The snowpack just got stressed overnight! Over 70cm fell last night at tree-line, bringing the weekly total to over 1.5m. Several weaknesses in the new snow can be found in the metre+ that lays above the persistent Dec 27th layer. The November and early Dec crusts and surface hoar layers may awaken with the rapid increase in load. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of snow, and strong wind from last few days have formed fresh wind and storm slabs. In most areas the mid and lower pack is well settled. Some areas have reports of buried surface hoar down 40-50 cm. It will be important to dig a pit to see if there is surface hoar in the region that you are skiing.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of storm snow since Jan 1 sits over a variety of surfaces including facets and surface hoar. Field tests throughout the region show easy to moderate results on this interface. Reactive wind slabs exist in alpine and some treeline locations. In most areas there is a well settled mid-pack over top of a weaker basal layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A total of 60cm settling storm snow since January 1st. Wind effect and slab formation on lee aspects in the alpine and treeline. This overlies buried surface hoar up to 2200m in sheltered areas as well as buried wind slabs on lee features at treeline and above. Well consolidated midpack. The bottom of the snowpack consists of depth hoar and facets</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">1.5m of new snow this week has altered the snowpack. Several weaknesses in the new snow can be found in the metre+ that lays above the persistent Dec 27th layer. Moderate to strong SW winds are redistributing the snow, creating slabs in alpine and tree-line lee features. Deep, loose snow in sheltered locations is available for power-sluffing.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cameron lakes received 40cm of new snow over the past 48h. Windslabs &amp; cornices are maturing creating the potential for larger avalanches as the load increases during the incoming storm on sunday. A crust down 10-30cm exists up to 1800m. The Middle of the snowpack is well settled but a weak facet/ melt freeze crust still lurks at base of snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of storm snow since Jan 1 sits over a variety of surfaces including facets and surface hoar. Field tests throughout the region show easy to moderate results on this interface. Reactive wind slabs exist in alpine and some treeline locations. In most areas there is a well settled mid and lower pack. Shallow regions have a weak lower layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of storm snow since Jan 1 sits over a variety of surfaces including facets and surface hoar. Field tests throughout the region show easy to moderate results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a well settled mid-pack over top of a weaker basal layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 60cm new snow since January 1st. Consistent SW winds creating wind slab on lee aspects in the alpine and treeline. This overlies buried surface hoar up to 2000m in sheltered areas as well as buried wind slabs on lee features at treeline and above. Well consolidated midpack. The bottom of the snowpack consists of depth hoar and facets.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">1.5m of new snow this week has significantly increased the load over the Dec 27th surface hoar. Within the new snow there are several triggerable interfaces from changes in wind, temp and crystal type. Recent SW winds have redistributed snow to alpine and treeline lees. Deep, loose snow in sheltered locations is sluffing fast in steep areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of storm snow since Jan 1 sits over a variety of surfaces including facets and surface hoar. Field tests throughout the region show easy to moderate results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a well settled mid-pack over top of a weaker basal layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Jan 1 sits over a variety of surfaces including facets, surface hoar and sun crust. Stability tests throughout the region show 'sudden' results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a well settled mid-pack over top of a weaker basal layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The area received 60cm new snow January 1-7. SW winds created wind slab on lee aspects and cross-loaded features the alpine and treeline. This overlies surface hoar up to 2000m in sheltered areas as well as buried wind slabs on lee features at treeline and above. The bottom of the snowpack consists of depth hoar and facets.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent snow has settled to around 80cm over the Dec 27th surface hoar or crust depending on aspect. Triggerable interfaces exist within that 80cm Including a thin crust 10-20cm above the Dec 27th layer. The mid and lower snowpack have been gaining strength but the load over early season crusts has increased significantly this week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extreme West winds yesterday have created a 10-60cm windslab sitting low in start zones on all but W aspects. New snow on top of this windslab produce small loose dry avalanches. A crust down 20-70cm exists up to 1800m. The middle snowpack is well settled in deep snowpack areas but a weak facet/ melt freeze crust still lurks at base of snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Jan 1 sits over a variety of surfaces including facets, surface hoar and sun crust. Stability tests throughout the region show 'sudden' results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a well settled mid-pack over top of a weaker basal layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Dec 31 sits over a variety of surfaces including facets, surface hoar and sun crust. Stability tests throughout the region show 'sudden' results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a settled mid-pack over top of weaker basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface faceting over previous wind effect in the ALP and TL lee and cross loaded features. This overlies a faceting and weakening mid-pack bridging basal facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent snow has settled to around 80cm over the Dec 27th surface hoar or crust depending on aspect and elevation. Triggerable interfaces exist within that 80cm, including a thin crust 10-20cm above the Dec 27th lyr. The mid and lower snowpack have been gaining strength but the load over early season crusts has increased significantly this week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Dec 31 sits over a variety of surfaces including facets, surface hoar and sun crust. Stability tests throughout the region show 'sudden' results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a settled mid-pack over top of weaker basal layers. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Dec 31 sits over a variety of surfaces including facets, surface hoar and sun crust. Stability tests throughout the region show </span><a href="https://www.facebook.com/ParksMountainSafety/?__xts__[0]=68.ARDrF2wzAtcFJgzgMfmzVIwjbtH5SX1s59lrGWtIT7FAI23rWKzc6RYteASQkDJgBuNv2jyRBKyW4QPNA3qT-xTim_YvkU7SSmw3oLKVqa4JcKIfQPt-TWEqEg_Lsj5WH5NyReaj8b3Z5bFK_xLfp_QIbPlY6Ty_asWwCxwXdvSABq7zUCY1Ug7D4TrhaZLftC3DH-5RSb8DRm9LHG4eGqEsacN_1wOPVBqPlblIBWiLnDkQlZXBEzWTDP4ttPRWNvSDL3463pxDAqR7b9UW6tGD_4DW7xY8D_yVaCbEo9YmINXMIbtdm3ESUg5v8fZsWBW08s-dKbd3eNT7jNqUxjwYJ3uBvFtNwvQQkw&amp;__xts__[1]=68.ARCdeQ-99HC9mNQSNQiNKMZP6QJyxVzZnf0fXRBxfr5X7oE7hcGrspryKYWCBZNz8iBfqgv3kkf_kCU-nC-1iCj93q9tUkS6rUBeQN0XHcS3X3VY-W1822hX7aVzpFgILGufHS9m4CayHeDmwRGWO3b_lBuy0bvppfdmRBUnPALjAGRe6tWfWzz4r84NCBm1tISS_UiWvTXhcx9QbZ7i9QbnrJJnsZ2GfdeY8GuQ7gSfWpznUPARRkRmuC-YnmKN00dcn7HHaDFw0IbP-oyA69_nvYz8EvtqtcN9t4NWaonGsDiMCdBsBO7NF8TrCSlm5LFiKrReasTh8QN3f7SP-i39laKbuYY9pvDGjg&amp;hc_ref=ARTYr8JnPXi6zYBt6tH-qhMY5CtDCwOlImpucd8zKIrMDgolz2pbQ7HY0DSjJTmQat8&amp;fref=nf&amp;__tn__=kC-R" target="_blank"><span class="s_9255B882">'sudden planar'</span></a><span class="s_AA239A9B"> results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a settled mid-pack over top of weaker basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface faceting at all elevations. Weakening midpack comprised of mixed forms and facets, bridging basal facets and DH. HS Average at TL: ~150cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Light to moderate winds have switched from NE to S over the past 24hrs, and have likely built fresh windslabs in immediate lees. Recent snowfall has settled to around 80cm over the Dec 27th surface hoar or crust depending on aspect and elevation. The mid and lower snowpack are generally well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-50 cm of light storm snow over a deteriorating windslab. New snow is producing loose dry avalanches in steep terrain but this will transition into surface Windslab Tues night. The Dec crust (present up to 1800m) is deteriorating with cold temps. The mid snowpack is well settled in deep areas but a weak facet/ melt freeze crust lurks at the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Dec 31 sits over a variety of surfaces including facets, surface hoar and sun crust. Stability tests throughout the region show </span><a href="https://www.facebook.com/ParksMountainSafety/?__xts__[0]=68.ARDrF2wzAtcFJgzgMfmzVIwjbtH5SX1s59lrGWtIT7FAI23rWKzc6RYteASQkDJgBuNv2jyRBKyW4QPNA3qT-xTim_YvkU7SSmw3oLKVqa4JcKIfQPt-TWEqEg_Lsj5WH5NyReaj8b3Z5bFK_xLfp_QIbPlY6Ty_asWwCxwXdvSABq7zUCY1Ug7D4TrhaZLftC3DH-5RSb8DRm9LHG4eGqEsacN_1wOPVBqPlblIBWiLnDkQlZXBEzWTDP4ttPRWNvSDL3463pxDAqR7b9UW6tGD_4DW7xY8D_yVaCbEo9YmINXMIbtdm3ESUg5v8fZsWBW08s-dKbd3eNT7jNqUxjwYJ3uBvFtNwvQQkw&amp;__xts__[1]=68.ARCdeQ-99HC9mNQSNQiNKMZP6QJyxVzZnf0fXRBxfr5X7oE7hcGrspryKYWCBZNz8iBfqgv3kkf_kCU-nC-1iCj93q9tUkS6rUBeQN0XHcS3X3VY-W1822hX7aVzpFgILGufHS9m4CayHeDmwRGWO3b_lBuy0bvppfdmRBUnPALjAGRe6tWfWzz4r84NCBm1tISS_UiWvTXhcx9QbZ7i9QbnrJJnsZ2GfdeY8GuQ7gSfWpznUPARRkRmuC-YnmKN00dcn7HHaDFw0IbP-oyA69_nvYz8EvtqtcN9t4NWaonGsDiMCdBsBO7NF8TrCSlm5LFiKrReasTh8QN3f7SP-i39laKbuYY9pvDGjg&amp;hc_ref=ARTYr8JnPXi6zYBt6tH-qhMY5CtDCwOlImpucd8zKIrMDgolz2pbQ7HY0DSjJTmQat8&amp;fref=nf&amp;__tn__=kC-R" target="_blank"><span class="s_9255B882">'sudden planar'</span></a><span class="s_AA239A9B"> results on this interface. Reactive wind slabs exist in alpine and some tree line locations. In most areas there is a settled mid-pack over top of weaker basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Dec 31 sits over a variety of surfaces including facets, surface hoar and sun crust. Windslabs may still exist in leeward alpine areas. In most areas there is a settled mid-pack over top of weaker basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface faceting at all elevations. Weakening midpack comprised of mixed forms and facets, bridging basal facets and DH. HS Average at TL: ~150cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Light to strong winds have switched from S to NE, over the past 24hrs, and have likely built fresh wind slabs in immediate lees. Recent snowfall has settled to around 80cm over the Dec 27th surface hoar or crust depending on aspect and elevation. The mid and lower snowpack are generally well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of snow since Dec 31 sits over a variety of surfaces including facets, surface hoar and sun crust. Windslabs may still exist in leeward alpine areas. In most areas there is a settled mid-pack over top of weaker basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 cm of new snow and sustained SW winds through Thursday will continue to build soft windslabs that trigger easily. This will make up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack which we expect to wake up again.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface faceting at all elevations. Weakening midpack comprised of mixed forms and facets, bridging basal facets and DH. HS Average at TL: ~150cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent winds from all directions have likely built fresh wind slabs in immediate lees. Faceting and cold temps have given surface snow a chalk-like feel underfoot. Recent snowfall has settled to around 80cm over the Dec 27th surface hoar or crust depending on aspect and elevation. The mid and lower snowpack are generally well settled and strong.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 cm of new snow and sustained SW winds through Thursday will continue to build soft windslabs that trigger easily. This will make up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack which we expect to wake up again.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 cm of new snow and sustained Southerly winds continue to build soft wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Light snowfall through the region over surface faceting. That faceting morphosis will be more pronounced in shallow HS areas. Upper pack settled and overlays a weakening mid-pack comprised of varied facet forms. This provides some questionable bridging over the basal facets and DH. HS average at TL: ~150cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of new snow sits atop soft wind slabs in exposed areas. The Dec 27th surface hoar/ crust layer is buried approximately 100cm. The mid and lower snowpack are generally well settled and strong.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued low density storm snow will present itself as blower pow over facetted snow down low, and windslab as you transition into treeline terrain. The December crust (present up to 1800m) is deteriorating with cold temps. The mid snowpack has been facetting with cold temperatures, and a weak facet/ melt freeze crust still lurks at the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 cm of new snow and sustained Southerly winds continue to build soft wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-15cm of new snow in the past 24 hrs and sustained Southerly winds continue to build wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued faceting of snowpack. Up to 15cm of new light dry snow is not bonding well to the upper settled pack. This overlies a weakening mid-pack comprised of varied facet forms. This provides some questionable bridging over the basal facets and DH. HS average at TL: ~145cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong southerly winds have redistributed 15cm of new storm snow. Reactive wind slabs have formed in exposed areas above treeline. The Dec 27th surface hoar/ crust layer is buried approximately 100cm. The mid and lower snowpack are generally well settled and strong.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25-40cm of recent storm snow remains light and fluffy in sheltered areas, but has been heavily wind affected at upper elevations by west winds, especially towards the divide. The midpack is facetted in the front ranges, but remains strong and well settled in the Cameron lake area. The base of the snowpack consists of a weak facet layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-15cm of new snow in the past 24 hrs and sustained Southerly winds continue to build wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-15cm of new snow in the past 24 hrs (highest amounts on Hwy. 93N)and sustained Southerly winds continue to build wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued faceting of snowpack. Up to 15cm of new light dry snow is not bonding well to the upper settled pack. This overlies a weakening mid-pack comprised of varied facet forms. This provides some questionable bridging over the basal facets and DH. HS average at TL: ~145cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong southerly winds have redistributed 15cm of new storm snow. Reactive wind slabs have formed in exposed areas above treeline. The Dec 27th surface hoar/ crust layer is buried approximately 100cm. The mid and lower snowpack are generally well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-15cm of new snow in the past 24 hrs (highest amounts on Hwy. 93N)and sustained S winds continue to build wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets/depth hoar near the base of the snowpack in thinner areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">  Warming temperatures and moderate to strong Southerly winds continue to build wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued faceting of snowpack. Up to 10cm of settled recent snow may not be bonding well to the upper settled pack. This overlies a weakening mid-pack comprised of varied facet forms. This provides some questionable bridging over the basal facets and DH. HS average at TL: ~135cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of low density snow overlies previous wind effect and surface facets from last weeks cold spell (this may be a reactive slab in isolated areas where it has been stiffened by the wind). The Dec 27th surface hoar/ crust layer is buried approximately 100cm. The mid and lower snowpack are generally well settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow paired with strong west winds has formed wind slabs at all elevations. The midpack is strong and well settled in the Cameron lake area, but that rapidly changes as you move east of the divide where you will find a weaker, shallower snowpack. The base of the snowpack consists of crusts and weak facets formed early in the season.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Warming temperatures and moderate to strong Southerly winds continue to build wind slabs in the alpine and open areas at tree line. There is up to 60 cm above the Dec 31 layer of facets, surface hoar and sun crust. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Warming temperatures and moderate to strong Southerly winds continue to build wind slabs in the alpine and at ridge tops at tree line. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Settled snow becoming more cohesive over previous surfaces, mostly facets. The upper snowpack has facetted and weakened; this is more pronounced in shallow HS areas where less than ~60cm. Inconsistent mid-pack bridging over the basal facets and DH. HS average at TL: ~135cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of settling storm snow lies on previous wind effect and small facets from last weeks cold (this may be a slab in areas where it has been stiffened by the wind). The mid and lower snowpack are generally well settled and strong. The Dec 27th surface hoar/crust persists down 100cm, but has not been reactive since the last major snowfall.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Warming temperatures and moderate to strong Southerly winds continue to build wind slabs in the alpine and at ridge tops at tree line. There is 40-70 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. In thin areas, concern remains for the weak layers of facets near the base of the snowpack.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Wind effect and isolated windslabs exist in lee areas in the alpine from recent loading. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The soft surface snow is becoming more cohesive and bonding to the previous surfaces as it settles with mild temperatures. The upper snowpack remains mainly facetted. This is pronounced in shallow areas where there is less than 60cm height of snow. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar. </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of settling storm snow lies on previous wind effect and small facets from last weeks cold. Variable soft slab can be found in the alpine at ridge-tops and immediate lee areas. The mid-lower snowpack is generally well settled and strong. The Dec 27th surface hoar/crust down 100cm has not been reactive since the last major snowfall.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Wind effect and isolated windslabs exist in lee areas in the alpine from recent loading. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Wind effect and isolated windslabs exist in lee areas in the alpine from recent loading. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The soft surface snow has become more cohesive and is bonding to the previous surfaces as it settles with mild temperatures. The upper snowpack remains mainly facetted. This is pronounced in shallow areas where there is less than 60cm height of snow. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar. </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of settling storm snow lies on previous wind effect and small facets from last weeks cold. Variable soft slab can be found in the alpine at ridge-tops and immediate lee areas. The mid-lower snowpack is generally well settled and strong. The Dec 27th surface hoar/crust down 100cm has not been reactive since the last major snowfall.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Wind effect and isolated windslabs exist in lee areas in the alpine from recent loading. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. Concern remains for the weak layers of facets and depth hoar near the base of the snowpack.</span></p>
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</style><p class="p_91E506DB"><span class="s_AA239A9B"> Fresh wind slabs (up to size 1.5) can be found near ridge-tops. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for deeper snow-pack areas which has a well settled lower pack.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The surface snow has become more cohesive and is bonding to the previous surfaces as it settles with mild temperatures. The upper snowpack remains mainly facetted particularly in shallow areas where there is less than 60cm height of snow. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar. </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Fresh storm slabs are building today, burying old wind slabs and facets from last week's cold temperatures. The mid-lower snowpack is generally well settled and strong. The Dec 27th surface hoar/crust down 100cm and currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme SW winds have formed wind slabs at all elevations. These windslabs have the potential to trigger weak layers deep in the snowpack during this warm period. The base of the snowpack consists of crusts and weak facets formed early in the season. The snowpack east of the divide is significantly shallower and inherently weaker.</span></p>
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</style><p class="p_91E506DB"><span class="s_AA239A9B"> Fresh wind slabs (up to size 1.5) can be found near ridge-tops. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. In most areas in Little Yoho the lower pack is well settled. Shallower snow-pack areas will see a weaker lower pack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for deeper snow-pack areas (over 2m) which have basal facets but not as prevalent.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is highly variable across the forecast area. The surface snow is becoming more cohesive and is bonding well. The upper snowpack remains mainly facetted, particularly in shallow areas where there is less than 60cm of snow. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm new snow in 24hrs has not yet bonded to the wind affected and facetted old surface below. 60cm of settled, progressively stiffer snow below that sits over a dense midpack. The Dec 27th surface hoar/crust is down 100cm, the Dec 11th surface hoar can still be found down 150cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 60+ cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for deeper snow-pack areas (over 2m) which have basal facets but not as prevalent.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for deeper snow-pack areas (over 2m) which have basal facets but not as prevalent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is highly variable across the forecast area. The surface snow is becoming more cohesive and is bonding well. The upper snowpack remains mainly facetted, particularly in shallow areas where there is less than 60cm of snow. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm new storm snow was accompanied by light to mod S winds and warm temperatures. Rain below 1000m yesterday. New snow overlies a strong midpack, with the exception of the Dec 27th surface hoar/crust down 100cm and the Dec 11th surface hoar down 150cm.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 40-60+ cm above the Dec 31 layer of facets, surface hoar and sun crust which is slowly becoming less reactive. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for deeper snow-pack areas (over 2m) which have basal facets but not as prevalent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces variable test results through the region. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is highly variable across the forecast area. The snowpack remains mainly facetted, particularly in shallow areas where there is less than 60cm of snow. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar. Today's moderate winds redistributing recent storm snow into lee features in the ALP/TL. </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun and thin cloud caused greenhouse effect yesterday with temps in sun exposed areas at treeline reaching +2'C. Expect a sun crust on solar aspects. Storm slabs from the ~60cm snow over the past week seem to be settling and bonding, but periods of moderate to strong southerly winds have created pockets of windslab on lee features. </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 40-60 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces variable test results through the region. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces variable test results through the region. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is highly variable across the forecast Region but, remains mainly facetted, particularly in shallow areas. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">~10cm of overnight snow has covered up yesterday's suncrust on solar aspects. Storm slabs from the ~60cm snow over the past week seem to be settling and bonding, but periods of moderate to strong southerly winds have created pockets of windslab on lee features, especially on northerly aspects.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent warm temperatures have settled the overall height of snow by 5-10%. A breakable crust exists up to 2000m and is more pronounced on solar aspects. In lee areas, a 20-70cm windslab sits over a very well settled midpack. The base of the snowpack is made up of a facet, melt freeze crust combo. The front range has significantly less snow.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent wind slabs can be found near ridge-tops. There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces variable test results through the region. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces test results in the hard range. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is highly variable across the forecast region but remains mainly facetted, particularly in shallow areas. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar. </span></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_AA239A9B { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B">Periods of moderate to strong southerly winds have created pockets of windslab on lee features, especially on northerly aspects. The mild temps are promoting settlement in the upper snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces test results in the hard range. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces test results in the hard range. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is highly variable across the forecast region but remains mainly facetted, particularly in shallow areas. There is inconsistent bridging in the mid-pack over the weak basal facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Periods of moderate to strong southerly winds have created pockets of windslab on lee features, especially on northerly aspects. The mild temps are promoting settlement in the upper snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces test results in the hard range. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind slabs are prevalent in the alpine and treeline. There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces test results in the hard range. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Today's extreme winds have created wind slab (Soft to hard) tree line and above. Most fetches are stripped. This overlies a weakening mid-pack comprised of varied facet forms. This provides some questionable bridging over the basal facets and DH. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">HS average at TL: ~145cm</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm of new snow overnight, coupled with moderate to strong winds likely formed storm slabs in cross loaded terrain and immediate lees. The mid and lower snowpack is well settled, all of our persistent weak layers are currently dormant; however, they will be tested on Friday and Saturday if we receive the 80mm of precip, high FL and strong wind.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Melt freeze crust up to 2000m. This surface crust will increase reactivity of storm snow arriving Fri/Sat. The upper snowpack consist of a 20-70cm windslab sitting over a well settled midpack. Strength of the snowpack will decrease with rising temps &amp; new snow. Upper snowpack avalanches have potential to entrain wet loose snow below freezing level.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind slabs are prevalent in the alpine and treeline. There is 40-80 cm above the Dec 31 layer of facets, surface hoar and sun crust which produces test results in the hard range. The bottom layer of the snow-pack consists of weak facets and depth hoar, except for in deeper snow-pack areas (over 2m) where the basal facets are not as prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind and storm slabs are developing over the next 24 hours with strong SW wind, 40-80 cm of snow, and rain below 2000 m. We expect this to overload the Dec 31 layer of facets, surface hoar and sun crust (currently down 40-80 cm) and/or the deep persistent basal layer. Loose wet avalanches are likely below tree line Saturday morning.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continuing strong SW winds have created wind slab (Soft to hard) tree line and above. Most fetches are stripped. This overlies a weakening mid-pack comprised of varied facet forms. This provides some questionable bridging over the basal facets and DH. HS average at TL: ~145cm Everything changes tonight with a 60cm storm forecasted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 10cm of new snow fell overnight with moderate S winds, adding to existing storm slabs in cross loaded terrain and immediate lees. The mid and lower snowpack is well settled, all of our persistent weak layers are currently dormant; however, they will be tested on Friday and Saturday if we receive the 75mm of forecasted precipitation.&nbsp; </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind and storm slabs are developing over the next 24 hours with strong SW wind, 40-80 cm of snow, and rain below 2000 m. We expect this to overload the Dec 31 layer of facets, surface hoar and sun crust (currently down 40-80 cm) and/or the deep persistent basal layer. Loose wet avalanches are likely below tree line Saturday morning.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind and storm slabs have developed with strong SW winds, 30 to 70 cm of snow above 2000m. Rain has soaked the snowpack at lower elevations.  The Dec 31 layer of facets, surface hoar and sun crust  is currently down 40-100 cm. The deep persistent basal layer sits 20 to 40 cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">40cm or more snow arrived in the storm in the past 24 hours with strong winds and warm temperatures. Expect thick storm slabs over the facetted midpack and weak basal facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm+ storm snow then a shift to rain below 2000m with strong S'ly winds will be destabilizing the upper snowpack. Extreme S'ly winds and snowfall will be forming storm slab well down lee slopes. with The mid and lower snowpack is well settled, our persistent weak layers are being tested by this warm storm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind and storm slabs have developed with strong SW winds, 30 to 70 cm of snow above 2000m. Rain has soaked the snowpack at lower elevations. The Dec 31 layer of facets, surface hoar and sun crust is currently down 40-100 cm. The deep persistent basal layer sits 20 to 40 cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 2000m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterdays intense storm brought Strong-Extreme winds (recorded gusts of up to 180km/hr), up to 70mm of precipitation, and a 12hr period of a 2000m freezing level.  Expect rugged travel with 10-15cm of snow on a crust below treeline, and windslab well into lees as well as huge fresh cornices at treeline and in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 2000m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 1800m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50 cm snow arrived  in Jan 31 / Feb 1 with&nbsp; strong winds and warm temperatures. The storm created thick storm slabs over the facetted midpack and weak basal facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We received 15-20cm of low density snow in the wake of Saturdays storm. This sits on firm surfaces from the Extreme winds, 70mm of precip, and 2000m freezing level mid storm. Expect rugged travel in all but smooth open slopes below treeline - with 10-15cm of snow on a crust- and pockets of windslab in lees at treeline and in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A thick melt freeze crust exists up to 2000m, capped by 5cm of new snow that has been transported by westerly winds. The alpine is highly wind affected by prevous west winds, with many windward areas completely stripped of snow, and lee areas containing wind slabs. The midpack is strong and well settled near the divide. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 1800m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 1800m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow, up to 50cm has blanketed much of the southern forecast region. Previous mid-pack bridging over deeper instabilities is supporting the new load over the basal facets and depth hoar. This new load and bridging has not been significantly field tested, treat the snowpack carefully. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We received 20-30cm of low density snow in the wake of Saturdays storm. This sits on firm surfaces resulting from the Extreme winds, 70mm of precip, and 2000m freezing level mid storm. Expect rugged travel in all but smooth open slopes below treeline, with 10-15cm of snow on a crust. Pockets of windslab exist in lees at treeline and in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 1800m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 1800m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 50 cm of snow fell during last weeks storm in the forecast region. Previous mid-pack bridging over deeper instabilities is supporting the new load over the basal facets and depth hoar. This new load and bridging has still not been significantly field tested, treat the snowpack with caution. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Yesterday's moderate wind produced wind slabs on immediate lees, and cross-loaded terrain features in the alpine and exposed areas of treeline. We have received 20-30cm of low-density snow since the atmospheric river event last weekend, which brought with it:70mm of precipitation, freezing levels to 2000m and extreme winds (to 181km/hr).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30 to 70 cm of recent storm snow at higher elevations, with a rain crust up to 1800m. Wind slabs exist in the alpine and exposed areas at tree line. The Dec 31 layer of facets, surface hoar and sun crust is currently down 50-100cm. The deep persistent basal layer sits 20 to 40cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to10cm of snow overnight brings the weekly total to 40-80cm. A rain crust up to1900m is now buried by 10-20cm of snow. Wind slabs exist in the alpine and at tree line. The Dec 31 layer of facets, surface hoar and sun crust is down 50-100cm. The deep persistent basal layer is ~30cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 50 cm of snow fell during last weeks storm in the forecast region. Previous mid-pack bridging over deeper instabilities is supporting the new load over the basal facets and depth hoar. This new load and bridging has still not been significantly field tested, treat the snowpack with caution. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued mod to strong winds have been producing soft slabs on immediate lees, and cross-loaded terrain features in the alp and exposed areas of TL. We have received 30cm+ of low-density new snow at treeline and above since the atmospheric river event last weekend. Expect dust on crust at lower elevations, and rugged travel.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong west winds have redistributed 5cm of recent snow, and scoured most areas below 2000m down to a thick melt freeze crust. The alpine is highly wind affected, with many windward areas completely stripped of snow and lee areas containing hard wind slabs. The midpack is well settled, though weaker basal facets can be found in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to10cm of snow overnight brings the weekly total to 40-80cm. A rain crust up to1900m is now buried by 10-20cm of snow. Wind slabs exist in the alpine and at tree line. The Dec 31 layer of facets, surface hoar and sun crust is down 50-100cm. The deep persistent basal layer is ~30cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to10cm of snow Wednesday gives 40-80cm since February. Wind slabs exist in the alpine.  A rain crust up to1900m is now buried by 10-20cm of snow.  The Dec 31 layer of facets, surface hoar and sun crust is down 50-100cm. The deep persistent basal layer is ~30cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 50 cm of snow fell Jan 31st to Feb 1st in the forecast region. SW winds are creating windslabs with the new snow. The mid-pack bridging over deeper instabilities is supporting the new load over the basal facets and depth hoar. This new load and bridging has not been field tested thus treat the snowpack with caution. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued moderate-strong winds have been producing soft slabs on immediate lees, and cross-loaded features in the alpine and exposed areas of TL. We have received 30+cm of low-density new snow at treeline and above since the atmospheric river event last weekend. Expect dust on crust and rugged travel on all but smooth slopes at lower elevations.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong west winds have redistributed 5cm of recent snow, and scoured most areas below 2000m down to a thick melt freeze crust. The alpine is highly wind affected, with many windward areas completely stripped of snow and lee areas containing hard wind slabs. The midpack is well settled, though weaker basal facets can be found in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to10cm of snow Wednesday gives 40-80cm since February. Wind slabs exist in the alpine. A rain crust up to1900m is now buried by 10-20cm of snow. The Dec 31 layer of facets, surface hoar and sun crust is down 50-100cm. The deep persistent basal layer is ~30cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20cm in the past 48 hrs gives 40-80cm since January 31. Wind slabs exist in the alpine. A rain crust up to1900m is now buried by 15-30cm of snow. The Dec 31 layer of facets, surface hoar and sun crust is down 50-100cm. The deep persistent basal layer is ~30cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 60 cm of snow fell Jan 31st to Feb 1st in the forecast region. SW winds are creating windslabs with the new snow. The mid-pack bridging over deeper instabilities is supporting the new load over the basal facets and depth hoar. This new load and bridging has not been field tested thus treat the snowpack with caution. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of low density snow overnight brings totals to 35+cm of snowfall since the atmospheric river event last weekend. Last nights snow overlies previous pockets of windslab from SW winds at upper elevations, and a thin suncrust on steep solar aspects. Expect dust on crust/rugged travel on all but smooth slopes at lower elevations.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20cm in the past 48 hrs gives 40-80cm since January 31. Wind slabs exist in the alpine. A rain crust up to1900m is now buried by 15-30cm of snow. The Dec 31 layer of facets, surface hoar and sun crust is down 50-100cm. The deep persistent basal layer is ~30cm above the ground and is more developed in shallow snowpack areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow in the past several days. Strong winds on Sunday created fresh wind slabs at treeline and in the alpine. In many areas a dense mid pack sits over the basal weak layers of facets and depth hoar. Deep snowpack areas (&gt;150 cm) have a denser base. A buried rain crust from February 1st is present up to 1850 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">SW winds have created deep pockets of windslab and pronounced cornice development on North aspects. Mixed slab character, support and sensitivity in the mid-pack is bridging the deeper basal facets and depth hoar. Average HS at treeline: ~160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate winds switching from north to south overnight have redistributed this week's 35+cm of low density snowfall. A thin suncrust exists down 10cm on steep solar aspects. Below 1800m, a melt-freeze up to 10cm thick is covered by 20-30cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow in the past several days. Strong winds on Sunday created fresh wind slabs at treeline and in the alpine. In thin snowpack areas a dense mid pack sits over basal weak layers of facets and depth hoar. Deep snowpack areas (&gt;150 cm) have a dense base with few weaknesses. A buried rain crust from February 1st is present up to 1850 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20 cm of snow in the past several days. Recent periods of strong wind have created fresh wind slabs at treeline and in the alpine. In many areas a dense mid pack sits over the basal weak layers of facets and depth hoar. Deep snowpack areas (&gt;150 cm) have a denser base. A buried rain crust from February 1st is present up to 1850 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">SW winds have created deep pockets of windslab and pronounced cornice development on North aspects. Mixed slab character, support and sensitivity in the mid-pack is bridging the deeper basal facets and depth hoar. Average HS at treeline: ~160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong variable winds across the park yesterday redistributed this week's low density 40cm. Possible thin sun crust on steep SW aspects is down ~20cm. Below 1800m, the Feb 1 Melt-freeze crust is down 30cm and observed up to 10cm thick at 1300m. Expect rugged travel in treed areas below 1200m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong variable winds across the park yesterday redistributed this week's low density 40cm. Possible thin sun crust on steep SW aspects is down ~20cm. Below 1800m, the Feb 1 Melt-freeze crust is down 30cm and observed up to 10cm thick at 1300m. Expect rugged travel in treed areas below 1200m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of recent snow with more in the forecast has formed new slabs with southwest winds. This sits on old wind slabs and a thick crust below 2000m that has locked up the lower snowpack. The midpack is well settled, though weaker basal facets can be found in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20 cm of snow in the past several days. Recent periods of strong wind have created fresh wind slabs at treeline and in the alpine. In many areas a dense mid pack sits over the basal weak layers of facets and depth hoar. Deep snowpack areas (&gt;150 cm) have a denser base. A buried rain crust from February 1st is present up to 1850 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20 cm of snow in the past several days. Strong wind has created fresh wind slabs at treeline and in the alpine up to 20cm thick today. In many areas a dense mid pack sits over the basal weak layers of facets and depth hoar. Deep snowpack areas (&gt;150 cm) have a denser base. A buried rain crust from February 1st is present up to 1850 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">SW winds have created variable windslab and pronounced cornice development on Northerly aspects and crossloaded features treeline and above. Suspect more sensitive soft slab developing at treeline.  The mid-pack is bridging the deeper basal facets and depth hoar. Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong SW winds are currently redistributing low density snow at ridge-top and exposed tree-line elevations. Variable soft slab should be expected in the immediate lee of ridges and across exposed alpine slopes. Below 1800m, the Feb 1 Melt-freeze crust is down 30cm and observed up to 10cm thick at 1300m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20 cm of snow in the past several days. Strong wind has created fresh wind slabs at treeline and in the alpine up to 20cm thick today. In many areas a dense mid pack sits over the basal weak layers of facets and depth hoar. Deep snowpack areas (&gt;150 cm) have a denser base. A buried rain crust from February 1st is present up to 1850 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of dry snow over the past 24-hours brings the 7-day storm total to 25-40 cm across the region. Light winds today kept the surface soft, but strong winds on Tues may have left some lingering wind slab in high alpine areas. We remain very concerned about the facetted weakness deep in the snowpack and continue to urge avoidance of start zones.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">SW winds have created variable windslab and pronounced cornice development on Northerly aspects and cross loaded features treeline and above. Suspect more sensitive soft slab developing at treeline. The mid-pack is bridging the deeper basal facets and depth hoar. Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Mild temps with light snowfall have created a soft, cohesive 10-20cm storm slab that overlies variable old surfaces. Recent mod/strong SW winds redistributed low density snow at ridge-top and exposed tree-line elevations; variable soft slab should be expected in these areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of dry snow over the past 24-hours brings the 7-day storm total to 25-40cm across the region. Light winds today kept the surface soft, but strong winds on Tues may have left some wind slab in high alpine areas. In the dry parts of the region we remain concerned about the facetted weakness deep in the snowpack; deep snowpack areas are strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of dry snow over the past 48-hours sits over top of a well settled mid-pack. The lower snowpack consists of weaker facets (particularly in shallower snowpack areas) that are producing moderate shears with snowpack tests. Isolated wind slabs exist near ridge tops and lee terrain in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Relentless SW winds continue building variable strength windslab and pronounced cornice development on Northerly aspects and cross loaded features treeline and above. Supportive mid-pack bridging the deeper basal facets and depth hoar. Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Mild temps with light snowfall have created a soft, cohesive 10-20cm storm slab that overlies variable old surfaces. Recent mod/strong SW winds redistributed low density snow at ridge-top and exposed tree-line elevations; variable soft slab should be expected in these areas. Solar input yesterday will have formed sun crust on steep S aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow has allowed for continued development of windslabs on all but West aspects. New &amp; old windslab sits over a thick melt freeze crust which exists up to 2100m. Recent natural windslab activity occurred with this melt freeze crust as the bed surface. The midpack is well settled, though weaker basal facets can be found in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of dry snow over the past 48-hours sits over top of a well settled mid-pack. In the deeper snowpack areas the lower snow-pack is well settled and displays no significant shears. In shallower areas the lower snow-pack is consists of weaker facets. Isolated wind slabs exist near ridge tops and in lee terrain at alpine elevations.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm over the last few days sits over top of a well settled upper and mid-pack. The lower snowpack (bottom 50cm) consists of weaker facets and depth hoar which are well preserved in areas under 150cm. These are still producing moderate shears with snowpack tests. Isolated wind slabs exist near ridge tops and lee terrain in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued SW winds continue building variable strength windslab and pronounced cornice development on Northerly aspects and cross loaded features treeline and above. A supportive mid-pack is bridging the deeper basal facets and depth hoar in some locations. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Average HS at treeline: ~180cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of storm snow overnight at our 1900m station with light to mod S-W winds. Expect new storm slab formation over previous wind effected snow as you transition into wind exposed terrain. Solar input Wednesday may have been sufficient to have form sun crust on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of snow over the last few days sits over top of a well settled mid-pack. In much of this deeper snowpack region, the lower snow-pack is well settled and displays no significant shears. Shallower snowpack areas will likely have more pronounced basal facets. Isolated wind slabs exist near ridge tops and in lee terrain at alpine elevations.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 35cm over the last few days sits over top of a well settled upper and mid-pack. The lower snowpack (bottom 50cm) consists of weaker facets and depth hoar which are well preserved in areas under 150cm HS. These are still producing moderate shears with snowpack tests. Isolated wind slabs exist near ridge tops and lee terrain in the alpine.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued Strong SW winds for the last 5 hours continue building variable strength windslab and pronounced cornice development on Northerly aspects and cross loaded features treeline and above. A supportive mid-pack is bridging the deeper basal facets and depth hoar in some locations. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">45cm of storm snow in 48hrs with light to mod S-W winds. Variable layers of resistance and sun crusts isolated to steep SW aspects reported within the storm snow over a strong snowpack of mostly rounds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 35cm of snow over the last few days has been redistributed by moderate to strong west winds TL and above. This sits over top of a well settled mid-pack. In much of this deeper snowpack region, the lower snow-pack is well settled and displays no significant shears. Shallower snowpack areas will likely have more pronounced basal facets. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect in the alpine with wind slabs at ridge tops and in lee areas. Up to 35cm of snow over the last few days sits over a well settled upper and mid-pack. In many areas the lower snowpack consists of weaker facets and depth hoar that are still producing moderate shears in snowpack tests. The Feb 1 crust is present below 1900m.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable strength windslab on the surface. Pronounced cornice development on northerly aspects and cross loaded features treeline and above. A supportive mid-pack is bridging the deeper basal facets and depth hoar in some locations. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm new snow overnight with moderate W wind. 95cm this week. Variable layers of resistance and sun crusts isolated to steep SW aspects reported within the storm snow over a strong snowpack of mostly rounds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some wind effect in the alpine with isolated wind slabs at ridge tops and in lee areas. Up to 40 of snow over the last few days sits over a well settled snowpack with lingering concerns for shallow areas where the basal facets are still present. The Feb 1 crust is present below 1900m and buried between 20 and 50 cm deep depending on the elevation.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued settlement and cool temperatures are slowly stabilizing the recently formed windslabs, which could still be triggered in steep, loaded areas in the alpine. Suspect sun crust formation on steep S and SW facing terrain. Weak, facetted snow near the base of the snowpack persists in much of the range, producing isolated but large avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable strength windslab on the surface. Pronounced cornice development on northerly aspects and cross loaded features treeline and above. The mid-pack is bridging the deeper basal facets and depth hoar in some locations. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 10cm of snow overnight, bringing the weekly total to 105cm at Fidelity. Variable stubborn wind slab was found in alpine elevations yesterday along ridge-tops and exposed tree-line features. Steep S to SW aspects have a suncrust buried anywhere between 30-60cm below the surface.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sheltered areas, such as Cameron Lake, are skiing well &amp; only have a few isolated pockets of windslab at ridgetop. Wind exposed areas have new &amp; old windslabs sitting over a melt freeze crust which exists up to 2200m. Reactivity of this crust is highly variable. The midpack is well settled, though weaker basal facets can be found in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued settlement and cool temperatures are slowly stabilizing the recently formed windslabs, which could still be triggered in steep, loaded areas in the alpine. Suspect sun crust formation on steep S and SW facing terrain. Overall the deep snowpack is strong in Little Yoho with no significant shear test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued settlement and cool temperatures are slowly stabilizing the recently formed windslabs, which could still be triggered in steep, loaded areas in the alpine. Suspect sun crust formation on steep S and SW facing terrain. Weak, facetted snow near the base of the snowpack persists in much of the range, producing isolated but large avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable strength windslab on the surface. Pronounced cornice development on northerly aspects and cross loaded features treeline and above. The mid-pack is bridging the deeper basal facets and depth hoar in some locations. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 10cm of snow overnight, bringing the weekly total to 115cm at Fidelity. Variable stubborn wind slab may be found in alpine elevations along ridge-tops and exposed tree-line features. Steep S to SW aspects have a suncrust buried anywhere between 30-60cm below the surface.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued settlement and cool temperatures are slowly stabilizing the recently formed windslabs, which could still be triggered in steep, loaded areas in the alpine. Suspect sun crust formation on steep S and SW facing terrain. Overall the deep snowpack is strong in Little Yoho with no significant shear test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued settlement and cool temperatures are slowly stabilizing the recently formed windslabs, which could still be triggered in steep, loaded areas in the alpine. Some sun crust formation on steep S and SW facing terrain. Weak, facetted snow near the base of the snowpack persists in much of the range, producing isolated but large avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable strength windslab on most surfaces TL and above. Some solar effect on steep South aspects. Pronounced cornice development on northerly aspects and cross loaded features treeline and above. The mid-pack is bridging the deeper basal facets and depth hoar in some locations. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Average HS at treeline: ~180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is 20-30cm of low density snow over a well settled mid-pack. Variable stubborn wind slab may be found in alpine elevations along ridge-tops and exposed tree-line features. Steep S to SW aspects have a suncrust buried anywhere between 30-60cm below the surface.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued settlement is slowly stabilizing any recently formed windslabs, which can still be triggered in steep, loaded areas in the alpine. Some sun crust formation on steep S and SW facing terrain. Overall the deep snowpack (observed as 3m+ in some areas) is strong in Little Yoho with no significant shear test results. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Fresh wind  slab development and continued cornice growth today in the alpine. Sun crust formation on steep S and SW facing terrain. Weak, facetted snow near the base of the snowpack persists in much of the range, producing isolated but large avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong sun followed by an overnight deep freeze left a crust on steep solar aspects.  On shaded slopes expect 20-30cm of low density snow over a well settled mid-pack.  Variable stubborn wind slab can be found in alpine elevations along ridge-tops and exposed tree-line features. Steep south aspects have a sun crust buried 30-60cm below the surface.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A sun crust is developing on solar aspects. In </span><a href="https://www.avalanche.ca/glossary?q=lee#leeward" target="_blank"><span class="s_9255B882">lee</span></a><span class="s_AA239A9B"> areas, multiple layers of windslab sit over the Feb 1st melt freeze crust which exists up to approx 2100m. Reactivity of this windslab is extremely variable. Expect windslabs to become more sensitive as temperature rises. The midpack is strong, though weaker basal facets can be found in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Fresh wind slab development and continued cornice growth in the alpine. Sun crust formation on steep S and SW facing terrain. Overall the deep snowpack (observed as 3m+ in some areas) is strong in Little Yoho with no significant shear test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued snow transport and cornice growth today in the high alpine. Sun crust formation on steep solar facing terrain. Weak, facetted snow near the base of the snowpack persists in much of the range, producing isolated but large avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable strength windslab on most surfaces treeline and above. Solar crusts on steep South aspects up to 2200m. Pronounced cornice development on northerly aspects and cross loaded features treeline and above. The mid-pack is bridging the deeper basal facets and depth hoar in some locations but there is allot of variability. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong sun followed by an overnight freeze will leave a crust on steep solar aspects. On shaded slopes expect 20-30cm of soft snow over a well settled mid-pack. Variable stubborn wind slab can be found in alpine elevations along ridge-tops and exposed tree-line features. Steep south aspects have a sun crust buried 30-60cm below the surface.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued snow transport and cornice growth today in the high alpine. Sun crust formation on steep solar facing terrain. Overall the deep snowpack (observed as 3m+ in some areas) is strong in Little Yoho with no significant shear test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued snow transport and cornice growth with winds affecting treeline ridge crests today. 5-10 cm of new snow now burying sun crusts isolated to steep solar facing terrain. Weak, facetted snow near the base of the snowpack persists in much of the range, producing isolated but large avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread hard slab on most surfaces treeline and above. Stripping any available snow from most windward alpine slopes and wind pressed or developing windslabs on lee aspects. Solar crusts on solar aspects up to 2500m. Cornice development on northerly aspects. The mid-pack is bridging the deep basal facets and depth hoar except in shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm+ storm snow has now buried the February 22 surface hoar layer. This layer is widespread accept on steep solar aspects where sun crust has formed. On shaded slopes expect 30cm of soft snow over a well settled mid-pack. Storm snow hides variable stubborn wind slab in exposed alpine elevations along ridge-tops and exposed tree-line features. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued snow transport and cornice growth with winds affecting treeline ridge crests today. 5-10 cm of new snow now burying sun crusts isolated to steep solar facing terrain. Weak, facetted snow near the base of the snowpack persists in much of the range, producing isolated but large avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15cm of snow in the last 48 hrs with moderate to strong alpine winds Saturday creating fresh wind slabs in lee areas. Isolated buried sun crusts exist on steep solar aspects. The Feb 1 crust is down 20-50cm and present below 1900m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread hard slab on most surfaces treeline and above. Scouring has occurred on windward alpine slopes and wind pressed or wind slabs on lee aspects. Solar crusts on solar aspects up to 2500m now buried by 5cm new snow. The mid-pack is bridging the deep basal facets and depth hoar except in shallow and steep rocky areas.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm+ storm snow has now buried the February 22 weak layer. This layer consists of surface hoar (observed up to 2300m) in sheltered areas and a sun crust on solar aspects. In some locations, the surface hoar may be sitting on a sun crust. On shaded slopes expect 30cm of soft snow over a well settled mid-pack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15cm of snow in the last 48 hrs with moderate to strong alpine winds Saturday creating fresh wind slabs in lee areas. Isolated buried sun crusts exist on steep solar aspects. The Feb 1 crust is down 20-50cm and present below 1900m. A dense snowpack with no significant weaknesses is present in most areas, but thin rocky areas have a faceted base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent storm snow covers previously formed wind slabs in lee areas, and buried sun crusts on steep solar aspects. The Feb 1 rain crust is down 20-50 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm new snow over the last 48 hours overlies wind slab and hard slab in the alpine, possible sun crust on steep solar aspects treeline and below. The southern section of the forecast region has a generally a more bridged midpack than the north around Marmot basin. Basal sections of the snowpack consist of up to 40cms of depth hoar and facets.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30+cm of storm snow has now buried the February 22 weak layer. This layer consists of surface hoar (observed up to 2300m) in sheltered areas and a sun crust on solar aspects. Surface hoar may be found on the sun crust in some areas. Where the new snow has become cohesive, it is reactive to human triggering as a 20-40cm soft slab. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of low density new snow sits on a variety of wind affected surfaces including previous windslab, suncrusts and the February 1 melt freeze crust, which exists up to approx 2100m. As winds increase this new snow will be blown into windslabs in lee areas. The midpack is strong, though weaker basal facets can be found in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent storm snow covers previously formed wind slabs in lee areas, and buried sun crusts on steep solar aspects. The Feb 1 rain crust is down 20-50 cm and present below 1900 m. A dense snowpack with no significant weaknesses is present in most areas, but thin rocky areas have a faceted base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent storm snow covers previously formed wind slabs in lee areas, and buried sun crusts on steep solar aspects. The Feb 1 rain crust is down 20-50 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses.&nbsp; </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Daily, trace amounts of new snow, spread irregularly over the region on old hard slab in the alpine. A thin sun/temperature crust on steep solar aspects at treeline and below. The southern forecast region has a supportive mid-pack. Less supportive and poor bridging over a pronounced basal weaknesses in the north; Whistlers/Portal and Maligne area</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30+cm of storm snow has now buried the February 22 weak layer. This layer consists of surface hoar (observed up to 2300m) in sheltered areas and a sun crust on solar aspects. Where the new snow has become cohesive, it is reactive to human triggering as a 20-40cm soft slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent storm snow covers previously formed wind slabs in lee areas, and buried sun crusts on steep solar aspects. The Feb 1 rain crust is down 20-50 cm and present below 1900 m. A dense snowpack with no significant weaknesses is present in most areas, but thin rocky areas have a faceted base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent storm snow covers previously formed wind slabs in lee areas, and buried sun crusts on steep solar aspects. The Feb 1 rain crust is down 20-50 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Daily, trace amounts of new snow, spread irregularly over the region on old hard slab in the alpine. A thin rain crust present on all aspects at treeline; 1700m and below. The southern forecast region has a supportive mid-pack. Less supportive and poor bridging over a pronounced basal weaknesses in the north; Whistlers/Portal and soon, Maligne area</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The February 22nd surface hoar layer is now buried 35-40cm. This layer is widespread up to 2300m. On solar aspects the surface hoar sits atop a crust. The surface snow is beginning to gain cohesion above this weak layer and in many places a soft slab had now formed. Incremental loading through February has created an otherwise benign mid-pack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of recent storm snow covers previously formed wind slabs in lee areas, and buried sun crusts on steep solar aspects. The Feb. 1 rain crust is down 20-50 cm and present below 1900 m. A dense snowpack with no significant weaknesses is present in most areas, but thin rocky areas have a faceted base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind effect in the alpine due to gusty SW winds. New wind slabs in lee areas. 10-20 cm of recent snow over buried sun crust on steep solar aspects. The Feb 1 rain crust is down 20-50 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Daily, trace amounts of new snow, spread irregularly over the region on old hard slab in the alpine. A thin rain crust present on all aspects at treeline; 1700m and below. The southern forecast region has a supportive mid-pack. Less supportive and poor bridging over a pronounced basal weaknesses in the north; Whistlers/Portal and soon, Maligne area</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong southerly winds and warmer temperatures have contributed to the formation of a soft slab on top of the February 22nd surface hoar layer, buried 35-40cm. This layer is widespread up to 2300m. On solar aspects the surface hoar sits atop a crust. Incremental loading through February has created an otherwise benign mid-pack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong westerly winds continue to develop windslabs in lee areas. Surface windslabs sit on a variety of surfaces including old windslab, suncrust &amp; the Feb.1 melt freeze crust. Expect windslabs to be more reactive on solar aspects particularly during warm temps on Friday. The midpack is strong, though weaker basal facets can be found in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some wind effect and new wind slabs in lee areas of the alpine. 10-20 cm of recent snow over buried sun crusts on steep solar aspects. The Feb. 1 rain crust is down 20-50 cm and present below 1900 m. A dense snowpack with no significant weaknesses is present in most areas, but thin rocky areas have a faceted base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind effect in the alpine due to gusty SW winds over the past week.  10-20 cm of recent snow over buried sun crust on steep solar aspects. The Feb 1 rain crust is down 20-50 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Daily, trace amounts of new snow redeposited at ridgetop with increasing winds, spread irregularly over the region on old wind slab in the alpine. The southern forecast region has a supportive mid-pack. Less supportive and poor bridging over a pronounced basal weaknesses in the north; Whistlers/Portal and soon, Maligne area</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread 3-7mm surface hoar layer on all aspects in combination with a 2-4cm sun crust was buried on February 22nd and now has up to 50cm of storm snow above it. This layer has been observed to 2450m. No other layers are currently active in the 3.5m snowpack of mostly rounded grains.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Some wind effect and new wind slabs in lee areas of the alpine. 10-20 cm of recent snow over buried sun crusts on steep solar aspects. The Feb. 1 rain crust is down 20-50 cm and present below 1900 m. A dense snowpack with no significant weaknesses is present in most areas, but thin rocky areas have a faceted base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of new snow with moderate SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up 20cm of new low density snow overlies a variety of surfaces including depending on aspect and elevation. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern part of the forecast region has a generally shallower snow pack that is less bridged above the basal facets and depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The February 22nd surface hoar (SH) layer lurks below 60cm+/- of storm snow. This layer is present on all aspects and consists of 3-7mm SH. On steep solar the SH sits on top of a 2-4cm sun crust. This layer has been observed to 2450m. No other layers are currently active in the 3.5m snowpack of mostly rounded grains.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of new snow with moderate SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m.  Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of new snow with strong SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up 15cm of storm snow overlies a variety of surfaces depending on aspect and elevation. New wind slabs forming on lee aspects. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern part of the forecast region has a generally shallower snow pack that is less bridged.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm of new snow came with strong SW winds yesterday and overloaded the February 22nd Persistent Weak Layer in many locations. This PWL is now buried 60+cm, and consists of 3-7mm surface hoar on all aspects up to 2450m and a crust on solar aspects. No other layers are currently active in the mid and lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow with strong SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m. Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to Extreme SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous storm snow overlies a variety of surfaces depending on aspect and elevation. New wind slabs forming on lee aspects. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern part of the forecast region has a generally shallower snow pack that is less bridged.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong gusting Extreme SW winds are building fresh windslabs in all open terrain. The February 22nd persistent weak layer is now buried down 60+cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. No other layers are currently active in the mid and lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Waterton received 15cm of snow Sunday with strong-extreme SW wind. This has added to a surface windslab which sits over a variety of surfaces including suncrust, old windslab &amp; the Feb.1 melt freeze crust. Recent rapid cooling has settled the upper snowpack significantly. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow with strong SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m. Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-30cm of new snow and Strong to Extreme SW continue to form wind slab at tree line and above. Watch for buried sun crust on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow overlies a variety of surfaces depending on aspect and elevation. New wind slabs forming on lee aspects. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern part of the forecast region has a generally shallower snow pack that is less bridged.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to Extreme SW winds have built windslabs in open terrain features at all elevations. The February 22nd persistent weak layer is now buried down 60-70cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. No other layers are currently active in the mid and lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow with strong SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m. Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-40 cm of storm snow in the past few days brings the weekly total to ~60cm. Strong to extreme Westerly winds continue to form storm/wind slab at all elevations. Watch for buried sun crust on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Thick snowpack areas have a denser base with few weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow overlies a variety of surfaces depending on aspect and elevation. New wind slabs forming on lee aspects. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern part of the forecast region has a generally shallower snow pack that is less bridged.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continuing Strong to Extreme SW winds are building windslabs in open terrain features at all elevations. The February 22nd persistent weak layer is now buried down 60-70cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. No other layers are currently active in the mid and lower snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The weekend will have a widespread &amp; reactive storm slab. As of Wednesday, strong-extreme SW winds with intermittent snowfall has aided windslab development. These fresh windslabs are well bonded to the multiple sun &amp; temperature crusts present in the upper snowpack. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">30-40 cm of storm snow in the past few days brings the weekly total to ~60cm. Strong to extreme Westerly winds continue to form storm/wind slab at all elevations. Watch for buried sun crust on steep solar aspects.</span><span class="s_AA239A9B"> Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Approximately 60 cm has fallen in the past week with strong to extreme Westerly winds creating widespread wind slabs. Watch for buried sun crust on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Isolated locations below 1900 m, the Feb 1 crust down may be starting to become reactive.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm of recent new snow overlies a variety of surfaces depending on aspect and elevation. Wind slabs are continuously forming on lee aspects. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern part of the forecast region is shallower and weaker. 20-30cm of snow may arrive Friday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface windslabs in open terrain features at all elevations. Some alpine bowls have been blasted by the winds while others appear barely touched. Wind effect is variable. Below these slabs, the Feb 22nd persistent weak layer is now buried down 60-70cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">Approximately 60 cm has fallen in the past week with strong to extreme Westerly winds creating widespread wind slabs. Watch for buried sun crust on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50-70 cm has fallen in the past week with strong Westerly winds. Expect to find wind slabs in lee areas and exposed terrain features. The recent snow is piling up and buries sun crust on steep solar aspects and the Feb 1 crust in isolated areas up to 1900m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">35cm of recent new snow overlies a variety of surfaces depending on aspect and elevation. The new snow is bonding well to the old surface. Wind slabs are continuously forming on lee aspects. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern part forecast region is shallower and weaker. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow is cloaking near surface windslabs in open terrain features at all elevations. Wind effect appears to be highly variable. Below these slabs, the Feb 22nd persistent weak layer is now buried down 60-70cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">50-70 cm has fallen in the past week with strong Westerly winds. Expect to find wind slabs in lee areas and exposed terrain features. The recent snow is piling up and buries sun crust on steep solar aspects and the Feb 1 crust in isolated areas up to 1900m. </span><span class="s_DDF6C5E8">Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50-70 cm has fallen in the past week with strong Westerly winds. Expect to find wind slabs in lee areas and exposed terrain features. The recent snow is piling up and buries sun crust on steep solar aspects and the Feb 1 crust in isolated areas up to 1900m. In thin snow pack areas a dense mid-pack sits over a weak, faceted base. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">35cm of recent new snow appears to be bonding well to the old surfaces. Wind transport has been continuously forming soft wind slab on lee aspects. The Columbia Icefields region has a well bridged mid pack overlying basal facets and depth hoar. The northern forecast region is weaker and shallow; bridging over the basal weakness is less reliable. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm+/- of storm snow with light winds covers recently formed windslabs in open terrain features at all elevations. Previous wind effect appears to be highly variable. Below these slabs, the Feb 22nd persistent weak layer is now buried down 50-80cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> 20cm of low density new snow has fallen in the park as of Saturday evening. This sits on previous windslabs above multiple sun &amp; temperature crusts present in the upper snowpack. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices are especially large in the Cameron lake Area.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">50-70 cm has fallen in the past week with strong Westerly winds. Expect to find wind slabs in lee areas and exposed terrain features. The recent snow is piling up and buries sun crust on steep solar aspects and the Feb 1 crust in isolated areas up to 1900m. Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-20 cm of snow Saturday night with light winds. Buried wind slabs are present in alpine lee areas. New sun crusts exist on steep solar aspects. 40-50 cm of recent snow sits over the Feb 29 crust interface on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base, while thick areas have a stronger base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate SW winds transporting available fetch to lee aspects forming new windslab and encouraging loose, dry releases from steep terrain through the region. The Icefields has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weaker and shallow; bridging over the basal weakness is less reliable, especially BTL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm+/- of storm snow has been redistributed by moderate S'ly winds near ridgecrests in the alpine and exposed treeline. Below these slabs, the Feb 22nd persistent weak layer is now buried down 50-80cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. In some locations, this surface hoar sits on a crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">5-10cm of snow Saturday night with light winds. Buried wind slabs are present in alpine lee areas. New sun crusts exist on steep solar aspects. 40-50 cm of recent snow over the Feb 29 crust interface on steep solar aspects. The buried Feb 1 crust is present up to 1900m. Generally this area has a deep dense snowpack, with over 300 cm in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the alpine the wind is starting to produce soft slabs in lee areas. New sun crusts exist on steep solar aspects. 40-50 cm of recent snow sits over the Feb 29 crust interface on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base, while thick areas have a stronger base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to Strong SW winds transporting available fetch to lee aspects forming new windslab and encouraging loose, dry releases from steep terrain through the region. The Icefields has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weak and shallow; bridging over the basal weakness is less reliable BTL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm+/- of storm snow has been redistributed by moderate S'ly winds near ridgecrests in the alpine and exposed treeline. Below these slabs, the Feb 22nd persistent weak layer is now buried down 60-90cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. In some locations, this surface hoar sits on a crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface snow is moist on solar aspects during the heat of the day. 20cm settling storm snow is being blown into windslabs by moderate SW winds, with windward ridgetops in the alpine stripped to rock. This sits on previous windslabs and crusts. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices are large and looming.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the alpine the wind is starting to produce soft slabs in lee areas. New sun crusts exist on steep solar aspects. 40-50 cm of recent snow sits over the Feb 29 crust interface on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak, faceted base, while thick areas have a stronger base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong winds on Tues and overnight Wed will have blown snow and created small windslabs directly beside ridge crests that are prone to human triggers. In some areas, this snow overlies buried sun crusts formed in late February. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme SW winds transporting available fetch to outer space and lee aspects forming new windslab low in start zones. The Icefields has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weak and shallow; bridging over the basal weakness is less reliable BTL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm+/- of storm snow has been redistributed by moderate southerly winds creating soft slabs in exposed areas. Below these slabs, the February 22nd persistent weak layer is now buried down 60-90cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects. 15cm of storm snow is expected to fall today. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong winds on Tues and overnight Wed will have blown snow and created small windslabs directly beside ridge crests that are prone to human triggers. In some areas, this snow overlies buried sun crusts formed in late February. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of snow Wednesday night has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow is bonding well to older snow surfaces. The Icefields has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weak and shallow; bridging over the basal weakness is less reliable BTL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25-30cm of snow and mod/strong SW winds last night has created a reactive storm slab. The new snow sits on a thin suncrust on solar aspects and small surface hoar on N'ly aspects. Below this slab, the Feb 22nd persistent weak layer is down 80-120cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15cm of snow Wednesday night has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of snow over the last 2 days has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> The Icefields area has a well bridged midpack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack above the basal facets and depth hoar.The fridge air will make for weak bonding of the new snowfall.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> Sun crusts are largely absent and the melt is evident in the valley bottom with rocks starting to appear. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25-30cm of snow and mod/strong SW winds in the last 48hrs has created a reactive storm slab. The new snow sits on a thin suncrust on solar aspects and small surface hoar on N'ly aspects. Below this slab, the Feb 22nd persistent weak layer is down 80-120cm, and consists of 3-7mm surface hoar on all aspects up to 2450m, and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Up to 20cm of new snow from convective flurries yesterday overlies wind affected surfaces including windslab and crusts from the extreme wind event earlier in the week. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices are large and looming. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of snow Wednesday night has been transported by moderate winds at upper elevations creating wind slabs on immediate lee slopes. On steep solar a thin crust has formed on the surface. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-25cm of snow over the last 3 days has been redistributed by moderate winds of variable direction at treeline and above creating wind slabs in open areas. On steep solar a thin crust has formed on the surface. We continue to monitor the deep, weak facetted snow in the shallower areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The Icefields area has a well bridged mid pack overlying basal facets and depth hoar.  3-5 cms new snow from pm Mar 12th blanketing Hs. The northern region is weaker with less bridging  midpack strength above basals and depth hoar.  Isolated strong NE valley winds in the townsite area stripping existing snowpack and reverse loading Alp/TL features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of storm snow on Tues night, that came in with mod to strong SW wind, is now settling over the Mar 10 interface of surface hoar on shaded slopes and suncrust elsewhere. Below this slab the Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m and a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> 15-25cm of snow over the last 3 days has been redistributed by moderate winds of variable direction at treeline and above creating wind slabs in open areas. On steep solar a thin crust has formed on the surface. The deep snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes. On steep solar aspects a thin sun crust is present. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong NE winds past 36 hrs stripping and redistributing upper snowpack. Wide spread scouring in exposed places. Hard slabs, soft slabs, sastrugi now present. The Icefields area has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack strength above basals and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong NE winds are building fresh windslabs in unusual places. The Mar. 10th interface of suncrust on all solar aspects and possibly small surface hoar on shaded slopes, is now buried down 20-40cms. The Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes. On steep solar aspects a thin sun crust is present. The deeper snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. On some steep solar aspects a thin sun crust is present. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A variety of wind affected surfaces. Wide spread scouring, stripping in exposed places. Hard slabs, soft slabs, sastrugi now present. The Icefields area has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack strength above basals and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong NE winds Friday-Saturday built windslabs in unusual places. The Mar. 10th interface of suncrust on all solar aspects and small surface hoar on shaded slopes, is now buried down 20-40cms. The Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20 cm of snow over the last several days has been redistributed by moderate winds from various directions (SW, N and E). New wind slabs are present in steep lee areas, with wind effect on many open slopes. On steep solar aspects a thin sun crust may be present. The deeper snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wide spread scouring, stripping in exposed places. Hard slabs and sastrugi now present. Sun Crust on S-SW aspects to ALP and Temperature crust on E-SW aspects TL and below. The Icefields area has a well bridged mid pack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack strength above basals weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Most open terrain is heavily wind effected from the strong NE winds Friday-Saturday. The Mar. 10th interface of a suncrust on all solar aspects, and isolated surface hoar, is now buried down 20-40cms. The Feb 22 persistent weak layer is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A sun crust is developing on the surface. Waterton received 40cm of snow in the townsite &amp; 20cm at Cameron Lake over the weekend. This storm was accompanied by easterly winds so expect </span><a href="https://www.avalanche.ca/glossary?q=rev#reverse-loading" target="_blank"><span class="s_9255B882">reverse loading</span></a><span class="s_AA239A9B">. The new snow is settling fast thanks to high daytime temperatures. The midpack is strong, though weaker basal facets still lurk in thin areas.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. The deeper snowpack of Little Yoho is generally quite strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, Surprisingly little activity noted recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong diurnal temperature swings have built a crust on solar aspects that will break down with daytime warming. Open terrain at upper elevations is heavily wind effected from the strong NE winds Friday-Saturday. The Feb 22 PWL is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. 15-20 cm of soft snow over a firm mid pack has been redistributed by moderate winds from various directions (SW, N and E). Wind slabs are present in steep lee areas, with wind effect on many open slopes above treeline. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. Widespread wind effect in the alpine from recent multidirectional winds with 5 cm new snow on top. On sheltered Northerly aspects there is 15-20 cm over a firm mid-pack.  In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The mornings can provide good travel on the melt freeze crust. By early afternoon the crust will start to break down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold nights and warm days have built a crust on slopes facing the sun. Expect this crust to break down with daytime warming. Open slopes at upper elevations are very wind effected from the strong NE winds Fri-Saturday. The Feb 22 PWL is down 90-130cm and consists of 3-7mm surface hoar on all aspects up to 2450m as well as a crust on solar aspects</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects. Widespread wind effect in the alpine from recent multidirectional winds with 5 cm new snow on top. On sheltered Northerly aspects there is 15-20 cm over a firm mid-pack. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snow accumulation over the last few days. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on steep solar aspects. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The mornings can provide good travel on the melt freeze crust. By early afternoon the crust will start to break down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crusts have formed on slopes facing the sun. These crusts will break down with daytime warming. Open terrain treeline and above has widespread wind effect from strong weekend winds. Cool overnight temperatures are starting to facet upper snowpack. The dormant Feb 22 surface hoar and crust combo is down 90-130cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5cm of recent snow distributed by L NE winds overlies a thick MFcr on solar aspects. North Faces are generally wind affected from previous strong northwest through northeast winds. The midpack is strong and well settled, though basal weaknesses exist in thinner snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">5-10cm of snow accumulation over the last few days. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on steep solar aspects. The deep snowpack of Little Yoho is generally strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snow that fell Wednesday now has a suncrust on solar aspects. Widespread wind effect in the alpine from recent multidirectional winds. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack continues to settle due to Diurnal conditions. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">The mornings can provide good travel on the melt freeze crust. By early afternoon the crust will start to break down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface has been affected by intense sun and the freezing level rising to at least 1900m yesterday. At treeline and above exposed terrain was heavily affected by the wind last weekend and varies from impenetrable to skis to punchy in places, especially where facetted by overnight cold temperatures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">5-10cm of snow accumulation over the last few days. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on steep solar aspects. The deep snowpack of Little Yoho is generally strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of snow that fell Wednesday now has a suncrust on solar aspects. Widespread wind effect in the alpine from recent multidirectional winds. In shallow snowpack areas the weak basal facets remain a concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A supportive Melt freeze crust now exists on all Solar aspects to Alpine elevation. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface has been affected by intense sun and the freezing level rising to at least 2100m yesterday. At treeline and above exposed terrain was heavily affected by the wind last weekend and varies from impenetrable to skis to punchy in places, especially where facetted by overnight cold temperatures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_DDF6C5E8">5-10cm of snow accumulation Wednesday. Widespread wind effect in the alpine from recent multidirectional winds. Sun crust on solar aspects. The deep snowpack of Little Yoho is generally strong with few weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-5 cm of new snow in eastern areas of the forecast region on Saturday night. Widespread wind effect in the alpine and down into treeline. Sun crusts on solar aspects and buried sun crusts on steep solar aspects. In thin snow pack areas a dense mid-pack sits over a weak faceted base, while deep snowpack areas have a solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasted snow (up to 5-8cm overnight Sunday) over a supportive melt freeze crust exists on all Solar aspects to Alpine elevation. Scoured from previous winds. Old hard slabs exists in the alpine and open tree line. More confidence in the southern snowpack. Cornices remain an overhead hazard, </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface crusts exist on all aspects to 1300m and on SE-W into the alpine. Surface hoar has been developing over the last few nights to 3mm with shady sheltered pockets in the trees up to 10mm. Wind affected surfaces in exposed tree line and the alpine vary from impenetrable to skis to punchy in places.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread wind effect in the alpine and down into treeline. Sun crusts on solar aspects and buried sun crusts on steep solar aspects. In most areas of the Little Yoho region a deep snowpack exists with few weaknesses, though thin areas still have a weak facetted base. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-10 cm of snow on Monday with the higher amounts in the west. Moderate SW winds in the alpine forming new wind slabs. Previous widespread wind effect in the alpine and treeline. Sun crusts and buried sun crusts on solar aspects. In thin snow pack areas a dense mid-pack sits over a weak faceted base, while deep snowpack areas have a solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Traces of new snow overnight on a supportive melt freeze crust exists on all aspects, BTL and solar aspects at TL and Alp elevations. Snowpack has yet to have a deep melt freeze cycle and basil weakness is still a looming hazard sensitive to large loads like your mum, and cornices.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface crusts exist on all aspects to 1300m and on SE-W into the alpine. Surface hoar has been developing over the last few nights to 3mm with shady sheltered pockets in the trees up to 10mm. Wind affected surfaces at tree-line and alpine elevations vary from breakable to rockhard/impenetrable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A supportive crust exists on the surface that will be buried by incoming snow. The exception is straight north facing slopes where new snow will fall on settled powder in sheltered areas, and wind slabs everywhere else. The mid pack is strong and well settled. Basal instabilities haven't been seen in some time, but are likely lurking in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-10 cm of snow at upper elevations on Monday. Moderate SW winds in the alpine forming new wind slabs. Previous widespread wind effect in the alpine and treeline. Sun crusts and buried sun crusts on solar aspects. In most areas of the Little Yoho region a deep snowpack exists with few weaknesses, though thin areas still have a weak facetted base. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moist new snow, more in the front ranges on a supportive melt freeze crust exists on all aspects, BTL and solar aspects at TL and Alp elevations. Snowpack has yet to have a deep melt freeze cycle and basil weakness is still a looming hazard sensitive to large loads like cornices.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of storm snow overlies a crust on solar aspects (SE through W) into the alpine. The new snow sits on surface hoar on shaded, polar aspects. Previously wind-affected surfaces at tree-line and alpine elevations vary from breakable to rockhard/impenetrable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20 cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The mid snowpack is consolidating providing good bridging strength over the weak base. Sun and temperatures crusts laminate the upper snowpack. At treeline and above watch for thin windslabs over these crusts where bonding may be poor, particularly on solar facing slopes. Cornices loom large and are particularly capricious at this time of year. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of storm snow overlies a crust on solar aspects (SE through W) into the alpine. The new snow sits on surface hoar on shaded, polar aspects. Previously wind-affected surfaces at tree-line and alpine elevations vary from breakable to rockhard/impenetrable.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm cm of light, dry new snow with minimal to no wind effect over the past 48-hours sits over a generally well settled and deep snowpack. In areas with less snow (&lt; 150 cm), a dense mid-pack overlies a facetted base while deep snowpack areas (&gt; 150 cm) have a strong, solid base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of storm snow has been redistributed by Moderate - Strong SW winds. This has created fresh windslabs which sit over a melt freeze crust on all but North aspects. The mid pack is strong and well settled. Basal instabilities haven't been seen in some time, but are likely lurking in thin areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable surface conditions exist with hard wind slabs in exposed locations and softer snow in more sheltered areas. The Nov 5 facet/crust combo is down 50-80 cm and producing variable test results, but can be 'sudden' in character. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Previous winds have stripped the snow from all fetch in the alpine and open tree line. Soft snow can still be found in specific sheltered locations at tree line and below. Snow depth at the Bald Hills at tree line is around 80cm with the Nov 4 crust down 50cm and breaking down. The snowpack is supportive to skis. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of new snow, and mod-strong winds have hidden a layer of surface hoar size 5-10mm in most sheltered areas of the park. Beneath this interface are old wind slabs in the Alpine and exposed areas of treeline. In sheltered areas around TL there is another buried layer of SH dwn 40-60-cm. The Nov 5th Cr is now buried over 1m down</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable surface conditions exist with hard wind slabs in exposed locations and softer snow in more sheltered areas. The Nov 5 facet/crust combo is down 50-80 cm and producing variable test results, but can be 'sudden' in character. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable surface conditions exist with hard wind slabs in exposed locations, softer snow in more sheltered areas and a surface crust on some solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-140 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Previous winds have stripped the snow from all fetch in the alpine and open tree line. Soft snow can still be found in specific sheltered locations at tree line and below. Snow depth at tree line is around 80cm with the Nov 4 crust down 50cm. The snowpack is supportive to skis. Suspect crust from the inversion on solar at treeline and lower alpine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of new snow, and moderate wind has hidden a widespread layer of surface hoar size 5-10mm in sheltered areas. Beneath this interface are old wind slabs in the Alpine and exposed areas of treeline. In sheltered areas around TL there is another buried layer of SH dwn 40-60-cm. The Nov 5th Cr is now buried over 1m down</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable surface conditions exist with hard wind slabs in exposed locations, softer snow in more sheltered areas and a surface crust on some solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-140 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable surface conditions exist with hard wind slabs in exposed locations, softer snow in more sheltered areas and a surface crust on some solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-140 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Previous winds have stripped the snow from all fetch in the alpine and open tree line creating slabs and crossloading gullies and depressions. Soft snow can still be found in specific sheltered locations at tree line and below. Snow depth at tree line is around 90cm with the Nov 4 crust down 50cm. Solar crust present steep SW terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A surface crust formed at treeline and above overnight on solar aspects. Where sheltered surface hoar has formed to sz 3. Widespread surface hoar 5-10mm is dn 10cm over old windslabs in the alpine and exposed areas of treeline. In sheltered areas around TL there is another buried layer of surface hoar dn 40-60-cm. Nov 5th Cr is down over 1m</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind transport has scoured SW aspects to ground in exposed alpine terrain. Northerly aspects &amp; protected areas have wind slab 5-40cm thick over a melt freeze crust. Lower snowpack is beginning to facet below this crust.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack @ 2000m: Cameron Lake 80cm. Less than 30cm in rest of park. Below tree line elevation is under </span><a href="https://www.avalanche.ca/glossary?q=threshold#threshold" target="_blank"><span class="s_9255B882">threshold </span></a><span class="s_AA239A9B">snowpack height.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable surface conditions exist with hard wind slabs in exposed locations, softer snow in more sheltered areas and a surface crust on some solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-140 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard wind slabs are present in exposed alpine locations with softer snow in sheltered areas. A sun crust is present on most steep solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Previous winds have stripped the snow from all fetches in the alpine and open tree line creating slabs and cross loading gullies and depressions. Soft snow can still be found in specific sheltered locations at tree line and below. Snow depth at tree line is around 90cm with the Nov 4 crust down 50cm. Solar crust present in steep SW terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">An overnight refreeze has left a crust on steep solar aspects in the alpine, which will break down by mid-day. Dry power sits on shaded aspects, though recent SW winds have created pockets of soft slab. Around TL there is a buried layer of surface hoar down 40cm. The Nov 5th crust is prominent, widespread, and sits under more than 1m of snow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard wind slabs are present in exposed alpine locations with softer snow in sheltered areas. A sun crust is present on most steep solar aspects. The Nov 5 facet/crust combo is down 50-120 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard wind slabs are present in exposed alpine locations with softer snow in sheltered areas. A sun crust is present on most steep solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Previous winds have stripped the snow from all fetches in the alpine and open tree line creating slabs and cross loading gullies and depressions. Warm temperatures have resulted in a melt freeze crust on solar aspects. Snow depth at tree line is up to 90cm with the Nov 4 crust down 50cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Overnight refreeze has left a crust on steep solar aspects at treeline and above, which will break down through the day. Dry power sits on shaded aspects. At TL, surface hoar on exists on the surface to sz 8.0mm, with a buried layer of surface hoar dn 40cm. The Nov 5th crust is prominent, widespread up to 2500m, and sits under more than 1m of snow </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard wind slabs are present in exposed alpine locations with softer snow in sheltered areas. A sun crust is present on most steep solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard wind slabs are present in exposed alpine locations with softer snow in sheltered areas. A sun crust is present on most steep solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Previous winds have stripped the snow from all fetches in the alpine and open tree line creating slabs and cross loading in gullies and depressions. Warm temperatures have resulted in a melt freeze crust on solar aspects. Snow depth at tree line is up to 90cm with the Nov 4 crust down 50cm. Basal weakness continue to develop.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The overnight refreeze has left a crust on steep solar aspects at treeline and above. Dry powder sits on shaded aspects. At TL and below, surface hoar exists on the surface to sz 8.0mm, with buried layers down 10cm (size 5-7mm) and down 40cm (size 3mm). The Nov 5th crust is prominent, widespread up to 2500m, and sits under more than 1m of snow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard wind slabs are present in exposed alpine locations with softer snow in sheltered areas. A sun crust is present on most steep solar aspects. The Nov 5 facet/crust combo is down 50-80 cm and producing hard to no results. This crust extends up to 2500 m on N aspects and higher on solar aspects. Snow depths at treeline are 70-130 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Welcome the Dec 8 layer, it should be a good one that we will all get to know. A mix of large surface hoar, sun crust, facets and old windslab from the clear skies will get buried overnight on Monday, pushed by strong to extreme winds. This will result in a short period of instability as the new snow will not bond well to all of these old grains.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">5cm new snow today with strong SW ridge winds burying a variety of surfaces including facets and isolated surface hoar TL and BTL, hard slab in the alpine and open TL, and solar crust on steep solar. Snow depth at tree line is up to 95cm with the Nov 4 crust down 50cm. Basal weakness continue to develop. An additional 25cm is expected overnight.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A surface crust on steep solar aspects is currently being buried by the incoming storm. Dry powder sits on shaded aspects. At TL and below, surface hoar exists on the surface to sz 8.0mm, with buried layers down 10cm (size 5-7mm) and down 40cm (size 3mm). The Nov 5th crust is prominent, widespread up to 2500m, and sits under more than 1m of snow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Welcome the Dec 8 layer, it should be a good one that we will all get to know. A mix of large surface hoar, sun crust, facets and old windslab from the clear skies will get buried overnight on Monday, pushed by strong to extreme winds. This will result in a short period of instability as the new snow will not bond well to all of these old grains.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30 cm of wet snow has been deposited on top of the Dec 8 layer of surface hoar, sun crust and facets and produces easy test results at the storm snow interface. This indicates a poor bond with the new snow. Over the next 24-hours this snow will settle into a more cohesive slab and the bond will not improve due to the weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 50cm of new snow in the past 24h with moderate SW winds has resulted in new winds slabs in ALP lee features and widespread storm slabs. These overlie a variety of previous surfaces including hard slabs in the ALP and open TL, facets and isolated surface hoar at TL and BTL, and solar crust on steep solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30+cm of warm snow and mod/strong SW winds have created a storm slab. It sits on a significant widespread surface hoar (SH) layer at tree-line and lower elevations. In the alpine, the storm slab rests on a crust on steep solar aspects. Several SH layers exist in the mid-upper pack, while the Nov 5 crust lurks as a deep persistent weakness.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind has scoured SW aspects to ground the alpine. A melt freeze crust is expected to form on solar aspects as freezing level drops with incoming storm on wed. Northerly aspects above 2000m have a wind slab sitting over a old melt freeze crust. 80cm of snow at Cameron Lake @2000m. Less than 20cm in rest of park. Below </span><a href="https://www.avalanche.ca/glossary?q=threshold#threshold" target="_blank"><span class="s_9255B882">threshold </span></a><span class="s_AA239A9B">at lower elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-30 cm of wet snow has been deposited on top of the Dec 8 layer of surface hoar, sun crust and facets and produces easy test results at the storm snow interface. This indicates a poor bond with the new snow. Over the next 24-hours this snow will settle into a more cohesive slab and the bond will not improve due to the weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-30 cm of low density new snow sits on the december 7th layer of sun crust, facets or surface hoar depending on your location. This new snow came with minimal wind and seems less reactive than we had thought it might be. At the bottom of the snowpack, the Nov. 5th crust / facet layer persists. Snowpack depths are 90-150 at treeline</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent HST along with moderate SW winds have resulted in new wind slabs in ALP lee features. The recent HST is settling and overlies a variety of surfaces, including hard slabs in ALP and open TL, facets and isolated surface hoar at TL and BTL, and crusts on steep solar aspects. The depth of the Nov 4th rain crust varies (down 40-100cm).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">35cm+ of warm snow and mod/strong SW winds have formed a storm slab. It sits on a significant widespread surface hoar (SH) layer at tree-line and lower elevations. In the alpine, the storm slab rests on a crust on steep solar aspects. Several SH layers exist in the mid-upper pack, while the Nov 5 crust lurks as a deep persistent weakness.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of low density new snow sits on the december 7th layer of sun crust, facets or surface hoar depending on your location. This new snow came with minimal wind. At the bottom of the snowpack, the Nov. 5th crust / facet layer persists, but has been less reactive in Little Yoho than BYK. Snowpack depths are 90-160 at treeline</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of low density new snow sits on the december 7th layer of sun crust, facets or surface hoar depending on your location. This new snow came with minimal wind and seems less reactive than we had thought it might be. At the bottom of the snowpack, the Nov. 5th crust / facet layer persists. Snowpack depths are 90-150 at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">40cm of storm snow from Dec 8th with moderate SW winds resulted in mainly ridgetop or exposed treeline wind slabs. The snow is settling. It overlies a variety of surfaces like hard slabs in the alpine and treeline, facets and isolated surface hoar at treeline, and crusts on steep solar aspects. The depth of the Nov 4th rain crust is 60-80cm down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Last weekend's surface hoar was modified by a freezing rain event Monday leaving a &lt;1cm crust as high as 2500m. Tuesday's warm storm brought 30cm+/- heavy snow that appears to bond well to the old snow surface. Field trip tests at 2100m on both S and N aspects gave Mod results in the storm snow and Mod to Hard results at the rain crust interface. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the Cameron lake area, 10-20cm of pristine low density storm snow sits on a newly formed crust. This overlies a well consolidated midpack above the 2020-11-05 ice crust that forms the bottom of the snowpack. Treeline snow depth in the Cameron lake area just over 1m with amounts tapering quickly at lower elevations and in other areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of low density new snow sits on the december 7th layer of sun crust, facets or surface hoar depending on your location. This new snow came with minimal wind and seems less reactive than we had thought it might be. At the bottom of the snowpack, the Nov. 5th crust / facet layer persists. Snowpack depths are 90-150 at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of low density snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. This snow came with minimal wind and is less reactive than we had thought it might be. The Nov. 5th crust / facet layer persists at the bottom of the snowpack. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">40cm of storm snow from Dec 8th remains soft, continues to stabilize and settle. Wind-slabs only formed at exposed ridgetop features. The new snow overlies a variety of surfaces ranging from firm snow to surface facets and crusts on steep solar aspects. The depth of the Nov 4th rain crust is 60-80cm down and caps basal facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of storm snow buried a variety of surfaces on Monday; surface hoar up to 10mm is rounding in some areas, localized freezing rain formed a crust in others while sunny breaks formed a crust on steeper solar aspects. Below that several surface hoar crust layers exist in the upper snowpack and the Nov 5 crust is down between 1m and 1.5m</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of low density snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. This snow came with minimal wind and is less reactive than we had thought it might be. The Nov. 5th crust / facet layer persists at the bottom of the snowpack. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of faceted snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. The Nov. 5th crust / facet layer persists at the bottom of the snowpack and continues to weaken over time. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">40cm of storm snow from Dec 8th remains soft, continues to stabilize and settle. Wind-slabs only formed at exposed ridgetop features. The new snow overlies a variety of surfaces ranging from firm snow to surface facets and crusts on steep solar aspects. The depth of the Nov 4th rain crust is 60-80cm down and caps basal facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of storm snow from Monday and Tuesday buried a variety of surfaces; surface hoar up to 10mm which is rounding in some areas; a localized thin crust from freezing rain in and around the Connaught creek drainage, and a crust on steeper solar aspects from sunny breaks. The Nov 5 crust is down between 1m and 1.5m</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the Cameron lake area, 10-20cm of faceted storm snow sits above a crust, and will be blow into new windslabs. A well consolidated midpack sits above a thick ice crust that forms the bottom of the snowpack. Treeline snow depth in the Cameron lake area just over 1m with amounts tapering quickly at lower elevations and in other areas of the park.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-40 cm of faceted snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. The Nov. 5th crust / facet layer persists at the bottom of the snowpack, but less prominent in deeper snowpack areas in Little Yoho. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Trace of new snow and light wind effect in the alpine. 20-40 cm of faceted snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. The Nov. 5th crust / facet layer persists at the bottom of the snowpack and continues to weaken over time. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">The storm snow is unconsolidated and faceting with the cold temps while overlying a variety of surfaces ranging from old hard wind slab, facets and crusts on steep solar aspects. The bottom of the snowpack is continuing to facet.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of storm snow from Monday and Tuesday buried a variety of surfaces; surface hoar up to 10mm which is rounding in some areas; a localized thin crust from freezing rain in and around the Connaught creek drainage, and a crust on steeper solar aspects from sunny breaks. The Nov 5 crust is down between 1m and 1.5m</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Trace of new snow and light wind effect in the alpine. 20-40 cm of faceted snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. The Nov. 5th crust / facet layer persists at the bottom of the snowpack but is less prominent in deeper snowpack areas of Little Yoho. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">From trace to 10cm new snow and light wind effect in the alpine. 20-40 cm of faceted snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. The Nov. 5th crust / facet layer persists at the bottom of the snowpack and continues to weaken over time. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Surface Hoar has been steadily growing on the previous storm snow, which is now unconsolidated and faceting with the cold temps. This overlies a variety of old surfaces ranging from hard wind slab, facets and crusts on steep solar aspects. The bottom of the snowpack is continuing to facet.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Traces of new snow and surface facetting continue to make for fast sluffing in steep terrain. Last weeks storm(30cm) buried a variety of surfaces; surface hoar up to 10mm (rounding in some areas); a thin crust from freezing rain in and around Connaught creek: and a stronger crust on steeper solar aspects. The Nov 5 crust is down between 1m and 1.5</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20cm of new snow and light wind effect in the alpine. 20-40 cm of snow sits on the Dec 7th layer of sun crust, facets or surface hoar depending on your location. The Nov. 5th crust / facet layer persists at the bottom of the snowpack and continues to weaken over time. Snowpack depths are 90-160cm at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The dominant issue in the snowpack is the 15-20 cm of low density storm snow and 20-25 cm of loose facets overtop of the Dec 7th layer of sun crust, facets or surface hoar. This snow is sluffing easily out of steep terrain. Winds are forecasted to increase on Wednesday creating fresh windslabs in open terrain. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Strong winds are creating wind slabs in the alpine and down into tree line. About 10cm of new snow, where not wind affected, is overlying surface hoar up to 2500m and widespread faced snow at all elevations. The snowpack is generally supportive despite facets and depth hoar at the base of the snowpack. The snowpack is 40-150cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">The lower and mid snowpack is relatively strong, with the Nov 5</span><sup><span class="s_A136FBD0">th</span></sup><span class="s_A136FBD0"> Cr currently unreactive to stability tests or skiers. The upper snowpack is stitched together by multiple surface hoar layers, including another one buried on DEC13th. New snow is slowly building a slab over the aforementioned SH layer, and could become reactive today, or tomorrow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The dominant issue in the snowpack is the 20-25 cm of low density storm snow and 20-25 cm of loose facets overtop of the Dec 7th layer of sun crust, facets or surface hoar. This snow is sluffing easily out of steep terrain. Winds are forecasted to increase on Wednesday creating fresh windslabs in open terrain. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The dominant issue in the snowpack is the 20-30 cm of low density storm snow and 20-25 cm of loose facets overtop of the Dec 7th layer of sun crust, facets or surface hoar. Continued winds are continuing to create fresh wind slabs in open terrain. Basal facets and crust are present and most pronounced in shallow areas. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Strong winds are creating wind slabs in the alpine and open treeline. The snowpack is generally supportive despite having a weaker, deep persistent base. Average depth is 55cm - 150cm depending on region and elevation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A136FBD0">Another 22cm of new snow brings our storm total to ~40cm in the last 48 hours. Strong winds from the Sth and mild temperatures have formed storm slabs at all elevations. Storm slabs have buried another Surface Hoar Layer (Dec 13th). The lower and mid snowpack is relatively strong, with the Nov 5th currently unreactive to stability tests or skiers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The dominant issue in the snowpack is the 20-30 cm of low density storm snow and 20-25 cm of loose facets overtop of the Dec 7th layer of sun crust, facets or surface hoar. Continued winds are continuing to create fresh wind slabs in open terrain. The Nov 5 facets and crust near the base of the snowpack are less pronounced in this area. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind slabs forming in the alpine with moderate to strong W winds. 20-50 cm of storm snow at treeline sits over the Dec 13 and Dec 7 layers of sun crust, facets and some surface hoar. The Nov crust/facets exist near the bottom of the snowpack and are weakest in shallow snowpack areas. Snowpack depths at treeline are between 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Strong SW winds are creating wind slabs in the alpine and open treeline. The mid snowpack is generally supportive with a weaker base consisting of facets and some locations depth hoar. Average depth is 55cm - 150cm depending on region and elevation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm+/- of new snow brings our storm total to ~50cm in the last 72hours. Mod S-SW winds and mild temperatures are forming soft storm slabs at all elevations. Weak layers; Dec 13 Surface Hoar and Dec 7 crust/Surface Hoar are in the top 60cm.  Deeper in the snowpack the Nov 5th  crust is currently unreactive to stability tests or skiers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At Cameron lake: 10-20cm of recent storm snow has been redistributed by strong SW wind. This has created new wind slabs which sit over a melt freeze crust. Expect the upper snowpack to become very reactive as new snow arrives on Sunday with rising temperatures. The mid snowpack is well consolidated with a ice crust forming the base of the snowpack. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind slabs forming in the alpine with moderate to strong W winds. 40-60 cm of storm snow at treeline sits over the Dec 13 and Dec 7 layers of sun crust, facets and some surface hoar. The Nov crust/facets exist near the bottom of the snowpack in shallow snowpack areas. Snowpack depths at treeline are between 100-180 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices growing and wind slabs forming in the alpine with moderate to strong W winds. 20-50 cm of storm snow at treeline sits over the Dec 13 and Dec 7 layers of sun crust, facets and some surface hoar. The Nov crust/facets exist near the bottom of the snowpack and are weakest in shallow snowpack areas. Snowpack at treeline is between 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">SW winds and new snow will continue to build wind slabs in the alpine and open treeline. Possible surface hoar down 25cm in sheltered locations treeline and below. The midpack is generally supportive with a weaker base consisting of facets and some locations depth hoar. Average depth is 65cm - 160cm depending on region and elevation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind, warmth and continued snowfall have formed a sensitive storm slab at all elevations over the Dec 13 surface hoar layer. Weak layers of concern are Dec 13 surface hoar down 45cm+ and Dec 7 crust/surface hoar layer down 65cm+. The Nov 5 crust has been unreactive to stability tests. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices growing and wind slabs forming in the alpine with moderate to strong W winds. 40-60 cm of storm snow at treeline sits over the Dec 13 and Dec 7 layers of sun crust, facets and some surface hoar. The Nov crust/facets exist near the bottom of the snowpack in shallow snowpack areas. Snowpack at treeline is between 100-180 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices growing and wind slabs forming in the alpine with moderate to strong W winds. 20-50 cm of storm snow at treeline sits over the Dec 13 and Dec 7 layers of sun crust, facets and some surface hoar. The Nov crust/facets exist near the bottom of the snowpack and are weakest in shallow snowpack areas. Snowpack at treeline is between 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 30cm of storm snow over last few days. SW winds continue to build wind slabs in the alpine and open treeline. Surface hoar down ~35cm in sheltered locations treeline and below. The midpack is generally supportive with a weaker base consisting of facets and some locations depth hoar. Avg depth is 65cm - 160cm depending on region and elevation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20+ cm of new snow, strong SW winds and warm temps continue to build a sensitive slab at all elevations. Weak layers of concern are Dec 13 surface hoar/facets down 60cm+ and Dec 7 crust/surface hoar layer down 75cm+. The Nov 5 crust lingers near the base of the snowpack but has been unreactive recently. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At Cameron lake: 25cm of storm snow has been redistributed by strong SW wind. This has created thick wind slabs which sit over the Dec 9th melt freeze crust. The mid snowpack is well consolidated with a ice crust forming the base of the snowpack. Treeline snow depth at Cameron lake up to 1.5m with amounts tapering quickly at lower elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cornices growing and wind slabs forming in the alpine with moderate to strong W winds. 20-50 cm of storm snow at treeline sits over the Dec 13 and Dec 7 layers of sun crust, facets and some surface hoar. The Nov crust/facets exist near the bottom of the snowpack and are weakest in shallow snowpack areas. Snowpack at treeline is between 80-160 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm of snow in the past 24hrs brings the storm total to 30-60cm. Winds slabs forming in the alpine down into tree line from strong West winds. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 35cm and ~65cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 50cm of low density storm snow over last few days. SW winds continue to build wind slabs in the alpine and treeline. Decomposing surface hoar down 30cm to 50cm in sheltered locations treeline and below. The midpack is generally supportive with a weaker base consisting of facets and depth hoar. Avg depth is 65cm - 160cm depending</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">26+ cm of new snow brings the 4 day storm total to over 1 meter! Strong S-SW winds and warm temps continue to build a sensitive slab at all elevations. The Dec 13 surface hoar/facets are down 90cm+ and the Dec 7 crust/surface hoar layer is down 100cm+. The Nov 5 crust lingers near the base of the snowpack but has been unreactive recently. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm of snow in the past 24hrs brings the storm total to 30-60cm. Winds slabs forming in the alpine down into tree line from strong West winds. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 35cm and ~65cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> 30-60 cm over the last week have been blown into windslabs in the alpine and down into tree line from strong West winds. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 35cm and ~65cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 50cm of low density storm snow over last few days. SW winds continue to build wind slabs in the alpine and treeline. Decomposing surface hoar down 30cm to 50cm in sheltered locations treeline and below. The midpack is generally supportive with a weaker base consisting of facets and depth hoar. Avg depth is 65cm - 160cm depending</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">125cm of snow over the last 5 days, along with strong S-SW winds and warm temps, has created a sensitive slab at all elevations. The Dec 13 surface hoar/facets are down 90cm+ and the Dec 7 crust/surface hoar layer is down 100cm+. The Nov 5 crust lingers near the base of the snowpack and several avalanches over the storm period stepped down to it. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60cm over the last week have been redistributed by strong west winds forming windslabs in exposed alpine and treeline areas. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 35cm and ~65cm respectively. The Nov crust/facets sit at the bottom of the snowpack and are generally well bonded. Height of snow at tree line is 80-150cm</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> An upslope storm dropped up to 35cm in Banff and Sunshine, and less (7-10cm) North and West. This was on top of 30-60cm over the last week. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">The snowpack continues to settle rapidly. NW winds continue to strip recently loaded lee slopes and build wind slabs in S-SE features. Decomposing surface hoar down 30cm to 50cm in sheltered locations treeline and below. The midpack is generally supportive with a weaker base consisting of facets and depth hoar. Avg depth is 65cm - 160cm depending</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">140cm of snow over the last 6 days, along with strong S-SW winds and warm temps, has created a sensitive slab at all elevations. The Dec 13 surface hoar/facets are down 140cm+ and the Dec 7 crust/surface hoar layer is down 150cm+. The Nov 5 crust lingers near the base of the snowpack and several avalanches over the storm period stepped down to it. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of new snow arrived with a moderate Northerly wind causing </span><a href="https://www.avalanche.ca/glossary?q=reverse#reverse-loading" target="_blank"><span class="s_9255B882">reverse loading</span></a><span class="s_AA239A9B">. New snow has a rain crust below 1900m within the storm slab. These new storm slabs sit over a thick persistent slab which overlies the Dec 9th melt freeze crust. The mid snowpack is well consolidated with a ice crust forming the base of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> A 10-15 cm over the last 24 hours which his was makes for 60+ cm over the last week in the region. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 60cm and ~90 cm respectively. The height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Winds from a variety of directions have blown the 30-60cm of snow from the past week into wind slabs at higher elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 40cm settled storm snow from last week is being pushed around by previous northerly winds and present SW winds TL and above. The new snow sits upon a facet layer with isolated surface hoar sheltered areas TL and below. The midpack is generally supportive with a weaker base consisting of facets and depth hoar. Avg depth is 65-160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">140cm of snow over the last 6 days, along with strong S-SW winds and warm temps, has created a sensitive slab at all elevations. The Dec 13 surface hoar/facets are down 140cm+ and the Dec 7 crust/surface hoar layer is down 150cm+. The Nov 5 crust lingers near the base of the snowpack and several avalanches over the storm period stepped down to it. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Winds from a variety of directions have blown the ~60cm of snow from the past week into wind slabs at higher elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Winds from a variety of directions have blown the 30-60cm of snow from the past week into wind slabs at higher elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A north wind event on Dec 22 loaded southerly lees; present strong to extreme SW winds are reloading northerly terrain with last weeks 40cm of storm snow. The new snow sits upon a facet layer with isolated surface hoar sheltered areas TL and below. Midpack is generally supportive with a weaker base of facets and depth hoar. Avg depth is 65-160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">120cm snow in the past week along with warm temps and strong S-SW winds culminating in slab formation at all elevation bands. Dec 13 surface hoar/facets are down 120cm+ and the Dec 7 crust/surface hoar layer is down 140cm+. The Nov 5 crust lingers near the base of the snowpack and several avalanches over the storm period stepped down to it.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of recent snow has been transported by strong SW-W winds. In the Cameron Lake area wind affect is less prevalent. A new rain crust (December 23) exists down 15cm below 1900m. Above this elevation, the December 9th melt freeze crust may remain a problem. The midpack is well consolidated with an ice crust forming the base of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Winds from a variety of directions have blown the ~60cm of snow from the past week into wind slabs at higher elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. Height of snow at tree line is 80-150cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent 25-45km/hr SW-W winds have blown the 30-60cm of snow from the past week into wind slabs at higher elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A north wind event on Dec 22 loaded southerly lees; present strong SW winds are reloading northerly terrain with last weeks 40cm of storm snow. The new snow sits upon a facet layer with isolated surface hoar in sheltered areas TL and below. The midpack is generally supportive with a weaker base of facets and depth hoar. Avg depth is 65-160cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm dropped 120cm snow accompanied by warm temps and strong S-SW winds. Slab formation is widespread. Weak layers; Dec 13 surface hoar/facets are down 70-110cm, Dec 7 crust/surface hoar layer is down 110-130cm+. The Nov 5 crust lingers near the base of the snowpack and several avalanches over the storm period stepped down to it.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent 25-45km/hr SW-W winds have blown the 30-60cm of snow from the past week into wind slabs at higher elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small amounts of new snow now bury wind slabs created by recent 25-45km/hr SW-W winds redistributing the 30-60cm of snow from the past week. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There is 15-30cm of soft snow or dense wind-slabs location dependent over a generally firm mid-pack. Mid-pack crusts on steep solar aspects may be encountered at tree-line and below. An early season crust is down 40-100cm and decomposing. It overlies weak basal facets and depth hoar but is well bridged by the mid-pack above unless shallow location.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm dropped 120cm snow and was accompanied by warm temps and strong S-SW winds, followed by strong N winds. Weak layers: Dec 13 surface hoar/facets are down 70-110cm, Dec 7 crust/surface hoar layer is down 110-130cm+. The Nov 5 crust lingers near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small amounts of new snow now bury wind slabs created by recent 25-45km/hr SW-W winds redistributing the 30-60cm of snow from the past week. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small amounts of new snow now bury wind slabs created by recent 25-45km/hr SW-W winds redistributing the 30-60cm of snow from the past week. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">15-30cm of soft snow or dense wind-slabs location dependent over a generally firm mid-pack. Dec. Surface Hoar is down 40cm in isolated sheltered spots and reactive to skier traffic. An early season crust is down 40-100cm and decomposing. It overlies basal facets and depth hoar but is well bridged by the mid-pack above unless shallow location.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Windslabs exist on ridge crests and exposed areas in the alpine and at treeline. In sheltered areas, the upper meter of the snowpack is generally 'right side up'. Weak layers: Dec 13 surface hoar/facets are down 70-110cm, Dec 7 crust/surface hoar layer is down 110-130cm+. The Nov 5 crust lingers near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snow depth is highly variable, with scoured windward slopes in the alpine, and windslab from SW winds. The Cameron Lake area has seen much less wind affect treeline and below. Dec 22 crust is down 5-20cm below 1900m, Dec 9 crust is not very prominent, down 20-80cm. The midpack is well consolidated with an ice crust forming the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small amounts of new snow now bury wind slabs created by recent 25-45km/hr SW-W winds redistributing the 30-60cm of snow from the past week. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small amounts of new snow now bury wind slabs created by recent SW-W winds redistributing the 30-60cm of snow from the past week. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">15-30cm of soft snow or dense wind-slabs location dependent over a generally firm mid-pack. Dec. Surface Hoar is down 40cm in isolated sheltered spots and reactive to skier traffic. An early season crust is down 40-100cm and decomposing. It overlies basal facets and depth hoar but is well bridged by the mid-pack above unless shallow location.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 25cm of recent snowfall has buried windslabs at upper elevations, and spotty surface hoar in sheltered areas below treeline. The upper snowpack is generally well bonded. Weak layers: Dec 13 surface hoar is down 70-110cm, Dec 7 crust/facte/surface hoar layer is down 110-130cm+. The Nov 5 crust lingers near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small amounts of new snow now bury wind slabs created by recent 25-45km/hr SW-W winds redistributing the 30-60cm of snow from the past week. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface conditions are soft, dry snow with isolated areas of wind effect at high elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and are strengthening. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">15-30cm of soft or dense snow (location dependent) over a generally firm mid-pack. Dec. Surface Hoar is down 40cm in isolated sheltered spots. An early season crust is down 40-100cm and decomposing. It overlies facets and depth hoar at the bottom of the snowpack but is well bridged by the mid-pack above unless found at shallow location.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 25cm of recent snowfall is being stiffened into a slab in some wind exposed areas. This new snow covers spotty surface hoar in sheltered areas at and below treeline. Weak layers persist down 70-110cm (Dec 13 surface hoar), and 110-130+cm (Dec 7 crust/facte/surface hoar).&nbsp; The Nov. 5th crust complex is near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snow depth is highly variable, and alpine and front range areas are very wind affected. The Cameron Lake area has seen much less wind treeline and below. The December 9 crust facet combo is down 30-80cm, still giving hard sudden results in test profiles. A sandwich of crusts and facets form the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface conditions are soft, dry snow with isolated areas of wind effect at high elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and are strengthening. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface conditions are soft, dry snow with isolated areas of wind effect at high elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and are strengthening. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Varied surface conditions with aspect and geographic location. 15-25cm of un-compacted snow over a firm mid-pack with facets and depth hoar lingering near the ground. Mid-December persistent layers, including SH, and SH/FC combos can be found down 25-40cm but, only in isolated and sheltered locations, and almost exclusively in the Icefields region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Approximately 25cm of new snow has fallen over the last few days, burying another surface hoar layer. Reports that the new snow is relatively right side up, with isolated storm slabs that are stubborn to trigger. This interface will become touchy in the coming days as it gets overloaded with storm snow and warm temperatures.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface conditions are soft, dry snow with isolated areas of wind effect at high elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and are strengthening. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface conditions are soft, dry snow with isolated areas of wind effect at high elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and are strengthening. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Light precipitation and winds over the day. 15-25cm of un-compacted snow over a firm mid-pack with facets and depth hoar lingering near the ground. Mid-December persistent layers, including SH, and SH/FC combos can be found down 25-40cm but, only in isolated and sheltered locations, and almost exclusively in the Icefields region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Approximately 20-30cm of new snow has fallen over the last few days, burying another surface hoar layer (Dec 25th). Reports that the new snow is relatively right side up, with isolated storm slabs that are stubborn to trigger. This interface will become touchy in the coming days as it gets overloaded with storm snow and warm temperatures.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A bit of fluff sits on a highly variable snowpack, and most areas have seen significant wind. The December 9 crust is down 30-80cm and is more prominent immediately around Cameron Lake, still giving hard sudden results in test profiles. A sandwich of crusts and facets form the base of the snowpack. Eastern areas hold a structurally weaker snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface conditions are soft, dry snow with isolated areas of wind effect at high elevations. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and are strengthening. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-170cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday the surface snow was soft with isolated areas of wind effect in the alpine. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and will be tested by the incoming snow load. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Light precipitation and strong SW winds through the day. 15-25cm of soft snow over a firm mid-pack with facets and depth hoar lingering near the ground. Mid-December persistent layers, including SH, and SH/FC combos can be found down 25-40cm but, only in isolated and sheltered locations, and almost exclusively in the Icefields region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A new surface hoar layer (Dec 26) is preserved, in isolated areas, under 30cm of recent snow. The Dec 13 surface hoar can still be found down 100cm and the Dec 7 crust down 120 with weaker, facetted snow between them. At the base of the snowpack are several early season crusts including the prominent Nov 5 with facets in between them.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday the surface snow was soft with isolated areas of wind effect in the alpine. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively and will be tested by the incoming snow load. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday the surface snow was soft with isolated areas of wind effect in the alpine. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 50cm new snow by Sun morning with mod/strong SW winds overlies 25-40cm of soft snow over a firm mid-pack with facets and depth hoar lingering near the ground. Mid-December persistent layers, including SH, and SH/FC combos can be found down 25-40cm but, only in isolated and sheltered locations, and almost exclusively in the Icefields region</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A new surface hoar layer (Dec 26) is preserved, in isolated areas, under 50cm of recent snow. The Dec 13 surface hoar can still be found down 100cm and the Dec 7 crust down 120 with weaker, facetted snow between them. At the base of the snowpack are several early season crusts including the prominent Nov 5 with facets in between them.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday the surface snow was soft with isolated areas of wind effect in the alpine. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. Height of snow at tree line is 120-200cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of new snow at treeline. Extensive wind effect in open areas at treeline and in the alpine. Wind slabs and new cornices are forming. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 120-180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">45cm HST seems to be bonding well to 25-40cm of soft snow over a firm mid-pack with facets and depth hoar lingering near the ground. Mid-December persistent layers, including SH, and SH/FC combos can be found down 40-60cm but, only in isolated and sheltered locations, and almost exclusively in the Icefields region</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">50cm of snow in the past 48hrs and strong to extreme winds from the SW, triggered a widespread avalanche cycle last night. A recent surface hoar layer (Dec 26) is preserved, in isolated areas, down 70+cm. The Dec 13 surface hoar can still be found down 100cm and the Dec 7 crust/facet/surface hoar (aspect/elevation dependent) layer is down 120cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of new snow at treeline. Extensive wind effect in open areas at treeline and in the alpine. Wind slabs and new cornices are forming. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50cm and ~80 cm respectively. The decomposing Nov crust/facets sits at the bottom of the snowpack. Height of snow at tree line is 130-200cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30 cm of storm snow at treeline. Extensive wind effect in open areas at treeline and in the alpine with wind slabs in lee areas. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50 cm and ~80 cm respectively. The decomposing Nov crust/facet layer sits at the bottom of the snowpack. Height of snow at tree line is 120-180cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">45cm of new snow further buries the mid-December persistent layers, (surface hoar and facet combo) down 40-70cm. The mid-pack is supportive where snow is deeper than 60cm. The bottom of the snowpack consists of facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">60cm of snowfall over the weekend was accompanied by strong to extreme winds from the SW. A surface hoar layer, buried Dec 26, may be preserved in sheltered areas at and below treeline, down 70+cm. The Dec 13 surface hoar can still be found down 120cm and the Dec 7 crust/facet/surface hoar (aspect/elevation dependent) layer is down 135+cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of recent storm snow has transitioned to wind slab in most areas. Fresh wind slabs sit over a persistent slab which rests on the Dec 9 crust. The Dec 9th crust is buried 30-80cm deep in the Cameron Lake area. Multiple crusts &amp; facets form the base of the snowpack. Areas east of the divide hold a thin and structurally weaker snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-30 cm of storm snow at treeline. Extensive wind effect in open areas at treeline and in the alpine with wind slabs in lee areas. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 70 cm and ~90 cm respectively. The decomposing Nov crust/facet layer sits at the bottom of the snowpack. Height of snow at tree line is 130-200cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of storm snow at treeline. Wind effect in open areas at treeline and in the alpine. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50 cm and ~80 cm respectively, sudden planar results in LIttle Yoho today and one explosive triggered size 2 in Sunshine area.  The Nov crust/facet layer sits at the bottom of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 45cm of new snow this past weekend is being redistributed by strong SW winds. This new snow has further buried the mid-Dec persistent layers (surface hoar and facet combo) down 40-70cm. The mid-pack is supportive where snow is deeper than 60cm. The bottom of the snowpack consists of facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">75cm of snowfall over the last 3 days was accompanied by strong to extreme winds from the SW. A surface hoar layer, buried Dec 26, is preserved in sheltered areas at and below treeline, down 70+cm. The Dec 13 surface hoar can still be found down 120cm and the Dec 7 crust/facet/surface hoar (aspect/elevation dependent) layer is down 135+cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of storm snow at treeline. Wind effect in open areas at treeline and in the alpine. The Dec 13 and Dec 7 sun crust/surface hoar/facet layers are down ~ 50 cm and ~80 cm respectively, sudden planar results in LIttle Yoho today and one explosive triggered size 2 in Sunshine area. The Nov crust/facet layer sits at the bottom of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm on Wed brings recent storm snow totals to 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some sheltered locations. Wind effect in open areas at treeline and in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">40cm of new snow from Sunday is being redistributed by SW winds mainly at exposed ridge-tops. This new snow overlies a sporadically distributed surface hoar and facet layer down 40-70cm. The mid-pack is supportive except in shallow locations. The bottom is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">In the past 4 days, 90cm of snow, SW winds, and mild temps have created a surface storm slab. This sits on a surface hoar layer, buried Dec 26, which is preserved in sheltered areas at and below treeline. The Dec 13 surface hoar can still be found down 120cm and the Dec 7 crust/facet/surface hoar (aspect/elevation dependent) layer is down 135+cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Upper elevations are heavily scoured but pockets of wind slab are building in lee and cross loaded terrain with significant cornice growth noted throughout the park. The Dec 9th crust was not reactive during last weeks natural avalanche cycle but large triggers may awaken this weakness. Areas east of the divide hold a thin &amp; faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm on Wed brings recent storm snow totals to 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some sheltered locations. Wind effect in open areas at treeline and in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm on Wed brings recent storm snow totals to 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some sheltered locations. Wind effect in open areas at treeline and in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">40cm of new snow from Jan 3rd continues to be redistributed by SW winds into wind-slabs mainly at exposed ridge-tops. This new snow overlies a sporadically distributed surface hoar and facet layer down 40-70cm. The mid-pack is supportive except in shallow locations. The bottom is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Rogers Pass has received approx 90cm of new snow at TL in 2021. This sits on a surface hoar layer, buried Dec 26, which is preserved in sheltered areas at and below treeline. The Dec 13 surface hoar can still be found down 120cm and the Dec 7 crust/facet/surface hoar (aspect/elevation dependent) layer is down 135+cm.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm on Wed brings recent storm snow totals to 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some sheltered locations. Wind effect in open areas at treeline and in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow totals are 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some locations. Wind effect in open areas in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results. The Nov. 5 basal crust/facets are currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">The top layer is 40cm of new snow from Jan 3rd which has settled down to 20-30cm in sheltered spots or was redistributed by SW winds into wind-slabs at higher elevations. It overlies a sporadically distributed surface hoar and facet layer down 40-70cm. The mid-pack is supportive except in shallow locations. The bottom is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have received approx 90cm of new snow at TL before the sunny skies took over. Expect wind affected snow on the surface in the alpine, and exposed areas of TL. This storm buries a SH layer (Dec 26), which is preserved in sheltered areas at and below treeline. The Dec 7/13th surface hoar/crust/facet sandwich is now 1.5m below the surface. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow totals are 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some locations. Wind effect in open areas in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow totals are 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some locations. Wind effect in open areas in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results. The Nov. 5 basal crust/facets are currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">The top layer is 40cm of new snow from Jan 3rd which has settled down to 20-30cm in sheltered spots or was redistributed by SW winds into wind-slabs at higher elevations. It overlies a sporadically distributed surface hoar and facet layer down 40-70cm. The mid-pack is supportive except in shallow locations. The bottom is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A thin crust formed yesterday on S and W aspects at all elevations and surface hoar 5mm in the shade to treeline. 90cm of recent snow has begun to settle. Dec 26 Surface Hoar is preserved down 80 in sheltered areas at and below treeline. The Dec 7th surface hoar/crust/facet layer is down 1.5m. Crusts and facets persist at the base of the snowpack</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Surface hoar is growing in most areas, but should be blown away by incoming winds. Upper elevations are heavily wind affected, and have recently grown throughout the park. The Dec 9th crust has not been reactive in the Waterton Region as of yet, but large triggers may awaken this weakness. Areas east of the divide hold a thin &amp; faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow totals are 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some locations. Wind effect in open areas in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results. The Nov. 5 basal crust/facets are currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow totals are 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some locations. Wind effect in open areas in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results. The Nov. 5 basal crust/facets are currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">The top layer is 40cm of new snow from Jan 3rd which has settled down to 20-30cm in sheltered spots or was redistributed by SW winds into wind-slabs at higher elevations. It overlies a sporadically distributed surface hoar and facet layer down 40-70cm. The mid-pack is supportive except in shallow locations. The bottom is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A thin surface crust on S and W aspects at all elevations and surface hoar 10mm in the shade to treeline. The Dec 26 surface hoar has been extremely hard to find down 70 on the old storm interface. The Dec 7th surface hoar/crust/facet layer is down 1.5m. Crusts and facets persist at the base of the snowpack</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent storm snow totals are 20-50 cm at treeline. This sits on a spotty stellar/surface hoar layer in some locations. Wind effect in open areas in the alpine. Two weak layers from early Dec persist 50-100 cm down. These have been generally unreactive but still giving hard sudden planar results. The Nov. 5 basal crust/facets are currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple cm's of new snow mixed with facets and surface hoar on the surface. Thin suncrust on some steep solar aspects. Wind effect in alpine areas. Three persistent weak layers from Dec are down 30-100 cm. These have generally been unreactive but occasionally result in hard sudden planar shears. The Nov. 5 basal crust/facets are currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Strong SW winds have been aggressively distributing surface snow on N through E aspects, at all elevations but especially in the alpine and open tree-line. The mid-pack is supportive except in shallow locations and regions like the Maligne range. The bottom is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow is covering a thin crust from sun and/or rime in exposed terrain, as well as surface hoar up to 10mm in the shaded areas at treeline and below. The Dec 26 surface hoar has been hard to locate down 70cm. The Dec 7th surface hoar/suncrust/facet layer is down 1.5m. Crusts (with some facetting) persist at the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple cm's of new snow mixed with facets and surface hoar on the surface. Thin suncrust on some steep solar aspects. Wind effect in alpine areas. Three persistent weak layers from Dec are down 30-100 cm. These have generally been unreactive but occasionally result in hard sudden planar shears. The Nov. 5 basal crust/facets are currently dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm snow coupled with strong S-SW winds may not bond well to underlying surfaces.  Below this, there are three persistent weak layers from Dec are down 30-100 cm that may become touchy with critical loading,  The Nov. 5 basal crust/facets may also become reactive with the in areas that receive rapid loading from the storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 40cm of snow is forecast overnight Tuesday into Wednesday accompanied by moderate to strong southerly winds.  The freezing level may reach 1600m; rain is likely at lower elevations.  The new snow will fall upon a supportive mid pack except regions with a shallow snowpack like the Maligne range. Basal snowpack is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of new snow is covering a thin crust from sun and/or rime in exposed terrain, as well as surface hoar up to 10mm in the sheltered areas at treeline and below. The Dec 26 surface hoar has been hard to locate down 70cm. The Dec 7th surface hoar/suncrust/facet layer is down 1.5m. Crusts (with some facetting) persist at the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Expect to find at least 30cm of new snow redistributed by strong SW winds, with a crust near the surface below 2000m. Upper elevations are heavily wind affected, and new windslabs will be found in lee areas. The Dec 9th crust can be found down 70-100cm at Cameron Lake. Areas east of the divide hold a thin &amp; faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm snow coupled with strong S-SW winds may not bond well to underlying surfaces. Below this, there are three persistent weak layers from Dec are down 30-100 cm that may become touchy with critical loading, The Nov. 5 basal crust/facets may also become reactive with the in areas that receive rapid loading from the storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of warm snow over the last 24 hours with strong west winds has created touchy windslabs in exposed locations and storm slabs in sheltered areas. This sits on three persistent weak layers from Dec down 30-100 cm that are likely more reactive than before. The Nov. 5 basal crust/facets may also be more sensitive in thin snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">25cm, and upwards of 55cm storm snow through the forecast region. Jan 12 interface is somewhat of a mystery, possibly a temp or rain crust, FC and/or SH with inconsistent reactivity. All over a supportive mid pack. Basal snowpack is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A 35-40cm storm slab is covering a thin crust from sun and/or rime in exposed terrain, as well as surface hoar up to 10mm in the sheltered areas at treeline and below. The spotty Dec 26 surface hoar is down 70-90cm. The Dec 7th surface hoar/suncrust/facet layer is down 1.5+m. Crusts with facets persist at the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Expect to find at least 30cm of new snow redistributed by strong SW winds, with wet snow freezing into a crust near the surface below 2000m. Upper elevations are heavily wind affected, and new windslabs will be found in lee areas. The Dec 9th crust can be found down 70-100cm at Cameron Lake. Areas east of the divide hold a thin &amp; faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of warm snow over the last 24 hours with strong west winds has created touchy windslabs in exposed locations and storm slabs in sheltered areas. This sits on three persistent weak layers from Dec down 30-100 cm that are likely more reactive than before. The Nov. 5 basal crust/facets may also be more sensitive in thin snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of recent snow with the incoming strong SW winds will form wind slabs in exposed locations. The top 120cm in the snowpack boasts 4 persistent layers. The Jan 11 surface hoar (6mm) is down 15-40cm and remains reactive where found. The Dec persistent layers are less reactive but produce sudden results when they fail.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">January 13th brought upwards of 55cm of new snow in the region. It has settled to 20-30cm with mild temperatures but being wind effected.&nbsp; The storm snow is uncertain but could be a temperature or rain crust or FC and/or SH with an inconsistent reactivity. The mid pack is supportive. Near the ground it is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A 40cm+ fresh storm slab covers a thin crust from sun and/or rime in exposed terrain. Sheltered terrain at and below treeline harbours surface hoar up to 10mm under the slab. The spotty Dec 26 surface hoar is down 70-90cm. The Dec 7th surface hoar/suncrust/facet layer is down 1.5m+. Crusts with facets persist at the base of the snowpack.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The storm brought 30cm of new snow. Upper elevations are heavily wind affected, and new windslabs will be found in lee areas. Below 1900m rain during the storm formed a breakable crust which can be found under 5cm of fluff. The Dec 9th crust can be found down 70-100cm at Cameron Lake. Areas east of the divide hold a thin &amp; faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of recent snow with the incoming strong SW winds will form wind slabs in exposed locations. The top 120cm in the snowpack boasts 4 persistent layers. The Jan 11 surface hoar (6mm) is down 15-40cm and remains reactive where found. The Dec persistent layers are less reactive but produce sudden results when they fail.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of recent snow has been redistributed in the alpine and open areas into treeline by mod to strong SW winds. The top 120cm in the snowpack displays 4 persistent layers. The Jan 11 surface hoar (6mm) is down 15-40cm and remains reactive where found. The Dec persistent layers are less reactive but produce sudden results when they fail.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">January 13th brought upwards of 55cm of new snow in the region. It has settled to 20-30cm with mild temperatures with continued wind slab development. The alpine has had continued strong winds promoting wind effect, wind slab formation and cornice growth. The mid pack is supportive. Near the ground it is weak facets and depth hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm dropped 40cm snow burying a thin crust from sun and/or rime in exposed terrain. Jan 10 surface hoar resides under the storm snow in sheltered terrain at and below treeline. The spotty Dec 26 surface hoar is down 70-90cm. The Dec 7th surface hoar/crust/facet layer is down 1.5m. Crusts with facets persist at the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of recent snow has been redistributed in the alpine and open areas into treeline by mod to strong SW winds. The top 120cm in the snowpack displays 4 persistent layers. The Jan 11 surface hoar (6mm) is down 15-40cm and remains reactive where found. The Dec persistent layers are less reactive but produce sudden results when they fail.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind effect in exposed alpine and treeline terrain. Thin sun crust on steep sheltered S aspects and a rain crust below 1500 m in eastern areas. Jan 11th interface down 15-30 cm with surface hoar found in isolated locations. Dec 25th, 13th and 7th layers are down 40-110 cm and generally produce hard or no results. Nov crust present near the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Jan 13th brought upwards of 55cm of new snow to the region and it continues to settle with mild temperatures. The alpine and wind prone treeline has had and will continue to have strong winds promoting wind effect, wind slab formation and cornice growth. The midpack is supportive. Near the ground it is weak facets and depth hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm dropped 40cm snow burying a thin crust from sun and/or rime in exposed terrain. Jan 10 surface hoar resides under the storm snow in sheltered terrain at treeline and below. The spotty Dec 26 surface hoar is down 70-90cm. The Dec 7th surface hoar/crust/facet layer is down 1.5m. Crusts with facets persist at the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind effect in exposed alpine and treeline terrain. Thin sun crust on steep sheltered S aspects. Jan 11th interface down 20-40 cm with surface hoar found in isolated locations. Dec 25th, 13th and 7th layers are down 50-120 cm and generally produce hard or no results. Nov crust present near the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10 cm of new snow over thin sun crust on steep solar aspects and over previously wind scoured terrain at treeline and above. Jan 11th interface down 20-35 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 50-120 cm and generally produce hard or no results. A rain crust exists on surface below 1500 m in eastern areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">30cm of unconsolidated surface snow continues to settle. The alpine and wind prone treeline has seen moderate/strong winds promoting wind effect, wind slab formation and cornice growth. The midpack is supportive. Spotty surface hoar can be found down 30cm and 70cm in sheltered and shaded locations below treeline</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10cm overnight covers a thin surface crust on steep solar aspects. The Jan 10 surface hoar is down 35-65cm in sheltered terrain at treeline and below and is capped by a thin freezing rain crust in some locations. The Dec 7th surface hoar/crust/facet layer is down 1.5m. Crusts with facets persist at the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15 cm of new snow over thin sun crust on steep solar aspects and over previously wind scoured terrain at treeline and above. Jan 11th interface down 30-40 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 60-120 cm and generally produce hard or no results. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10 cm of new snow over thin sun crust on steep solar aspects and over previously wind scoured terrain at treeline and above. Jan 11th interface down 20-35 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 50-120 cm and generally produce hard or no results. A rain crust exists on surface below 1500 m in eastern areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">30cm of unconsolidated surface snow continues to settle. The alpine and wind prone tree line areas have seen a lot of moderate to strong winds promoting wind effect, wind slab formation and cornice growth. The midpack is supportive. Spotty buried surface hoar can be found down 30cm and 70cm in sheltered and shaded locations below treeline</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-20cm covers a thin surface crust on steep solar aspects. Wind slab in Alp/TL lee features. The Jan 10 surface hoar is down 35-65cm in sheltered terrain at tree-line and below and is capped by a thin freezing rain crust in some locations. The Dec 7th surface hoar/crust/facet layer is down 1.5m. Crusts with facets at the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There is a surface melt freeze crust up to 1900m on all aspects. Recent storm was accompanied by strong to extreme Westerly wind creating stiff Wind Slabs in lee areas. Multiple layers of wind slab sit over the Dec 9th crust which can be found down 70-100cm near Cameron Lake. Areas east of the divide hold a thin &amp; faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10 cm of new snow over thin sun crust on steep solar aspects and over previously wind scoured terrain at treeline and above. Jan 11th interface down 20-35 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 50-120 cm and generally produce hard or no results. A rain crust exists on surface below 1500 m in eastern areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10 cm of snow over thin sun crust on steep solar aspects and over previously wind scoured terrain at treeline and above. Jan 11th interface down 20-35 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 50-120 cm and generally produce hard or no results. A rain crust exists on surface below 1500 m in eastern areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">30cm of unconsolidated surface snow continues to settle. Wind event in progress. Strong to X southwest winds stripping exposed terrain and continuing to promote wind effect, wind slab formation and cornice growth. The midpack is supportive. Spotty buried surface hoar can be found down 30cm and 70cm in sheltered and shaded locations below tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable snow surface, including a thin suncrust on steep S/SW asp, isolated soft slab at ridge top, and light powder on sheltered slopes. The Jan 10 surface hoar is down 35-65cm in sheltered terrain at tree-line and below. The Dec 7th surface hoar/crust/facet layer is down 1.5m. Crusts with facets at the base of the snowpack. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10 cm of snow over thin sun crust on steep solar aspects and over previously wind scoured terrain at treeline and above. Jan 11th interface down 20-35 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 50-120 cm and generally produce hard or no results. A rain crust exists on surface below 1500 m in eastern areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme winds overnight redistributed 10cm of snow into immediate lee windslabs. Jan 11th interface down 20-35 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 50-120 cm and generally produce hard or no results. A rain crust exists on surface below 1500 m in eastern areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Strong to extreme winds have stripped snow from exposed terrain and fetch areas and resulted in wind slabs and wind affected snow in open terrain below treeline, at treeline and in the alpine. The midpack is supportive. Surface hoar is found down 40cm to 80cm in isolated sheltered locations.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong winds, and a little bit of new snow overnight has created wind slabs in exposed terrain features in the Alpine and at Tree Line. The new snow sits on a variety of surfaces, including but not limited to a thin sun crust on steep S/SW asp, and SH. The Jan 10 layer is down 40-60cm in sheltered terrain at tree-line and below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme winds overnight redistributed 10cm of snow into immediate lee windslabs. Jan 11th interface down 20-35 cm producing mod to hard results. Dec 25th, 13th and 7th layers down 50-120 cm and generally produce hard or no results. A rain crust exists on surface below 1500 m in eastern areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A generally strong snowpack exists with several surface hoar layers visible in the upper meter, but they don't produce test results. Significant wind effect (ie: blasted) in all alpine areas and expect the odd isolated, hard windslab to linger in steep loaded areas in the high alpine. Soft surface snow remains just below ridge crests at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Strong to extreme southwesterly winds have stripped snow from exposed terrain and fetch areas and resulted in wind slabs and wind affected snow in open terrain below treeline, at treeline and in the alpine. The midpack is supportive. Surface hoar is found down 40cm to 80cm in isolated sheltered locations.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous strong to extreme southerly winds has had widespread wind effect in the Alpine and at Tree Line. In sheltered locations one can find low-density storm snow on the surface; however wind scouring and hard slabs are the norm in many locations at and above TL. The Jan 10 layer is down 40-60cm in sheltered terrain at tree-line and below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_E6FD2046">Upper elevations are heavily wind affected, and reactive windslabs can be found in isolated lee areas. Below 1900m a breakable crust exists making skiing challenging. The Dec 9th crust can be found down 70-100cm at Cameron Lake. Areas east of the divide hold a thin &amp; faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A generally strong snowpack exists with several surface hoar layers visible in the upper meter, but they don't produce test results. Significant wind effect (ie: blasted) in all alpine areas and expect the odd isolated, hard windslab to linger in steep loaded areas in the high alpine. Soft surface snow remains just below ridge crests at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep loaded areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting. This has diminished the sensitivity of wind slabs, and rendered the four layers of surface hoar visible in the upper meter, as dormant..</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There are no significant changes in the snowpack over the past 3 days. Previous winds have stripped snow from exposed terrain and resulted in wind slabs and wind affected snow in open terrain below treeline, at treeline and in the alpine. The midpack is supportive. Surface hoar is found down 40cm to 80cm in isolated sheltered locations.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme southerly winds created widespread wind effect in the Alpine and at Tree Line, characterized by areas of scouring as well as localized hard slabs. In sheltered locations one can find low-density storm snow on the surface. The Jan 10 surface hoar/ crust layer is down 40-60cm in sheltered terrain at tree-line and below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep loaded areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting. This has diminished the sensitivity of wind slabs, and rendered the four layers of surface hoar visible in the upper meter, as dormant..</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep loaded areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting. This has diminished the sensitivity of wind slabs, and rendered the four layers of surface hoar visible in the upper meter, as dormant..</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Frigid temperatures is creating surface facets. Previous strong to extreme winds have stripped snow from all exposed terrain creating a lot of hard wind slabs and wind affected snow in open terrain below treeline to the alpine. The midpack is supportive. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme southerly winds created widespread wind effect in the Alpine and at Tree Line. The wind created scouring as well as localized hard slabs and cornice growth. Recently formed cornices may be fragile. Steep solar slopes are now topped with a thin sun crust. In sheltered locations one can find low-density storm snow on the surface. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep loaded areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting. This has diminished the sensitivity of wind slabs, and rendered the four layers of surface hoar visible in the upper meter, as dormant..</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep lee areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting and this has diminished the sensitivity of wind slabs...and rendered the four layers of surface hoar visible in the upper meter dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Continued surface faceting with cooler temperatures. Previous strong to extreme winds have stripped snow from all exposed terrain creating a lot of hard wind slabs and wind affected snow in open terrain below treeline to the alpine. The midpack is supportive. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temps have facetted and softened previous wind effect from extreme southerly winds. Cold has also weakened cornices which have grown substantially during the past couple of storms. Surface hoar growth has been observed in to the alpine. Steep solar slopes have a thin sun crust. And, low density snow (good skiing) persists in sheltered areas.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep lee areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting and this has diminished the sensitivity of wind slabs...and rendered the four layers of surface hoar visible in the upper meter dormant.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep lee areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting and this has diminished the sensitivity of wind slabs and rendered the four layers of surface hoar that exist in the upper snowpack dormant.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Surface faceting continues with cooler temperatures. Previous strong to extreme winds have stripped snow from all exposed terrain creating a lot of hard wind slabs and wind affected snow in open terrain below treeline to the alpine. The midpack is supportive. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Cold temps have facetted and softened previous wind effect from extreme southerly winds. Cold has also weakened cornices which have grown substantially during the past couple of storms. Surface hoar growth has been observed in to the alpine. Steep solar slopes have a thin sun crust. And, low density snow (good skiing) persists in sheltered areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Upper elevations are heavily wind affected, and generally quite hard. Reactive windslabs may be found in isolated lee areas. Below 1900m a crust exists that varies from bulletproof to breakable dependent on aspect and elevation. Areas east of the divide hold a thinner and more faceted snowpack, with more potential for surprises in alpine areas.</span></p>
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.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep lee areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting and this has diminished the sensitivity of wind slabs and rendered the four layers of surface hoar that exist in the upper snowpack dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep lee areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting and this has diminished the sensitivity of wind slabs and rendered the four layers of surface hoar that exist in the upper snowpack dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Surface faceting continues with cooler temperatures. Previous winds have stripped snow from all exposed terrain creating hard wind slabs and wind affected snow in any open terrain. The mid-pack is supportive. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Little change, other than continued facetting and softening of previous wind effect from extreme southerly winds. Cold-weakened cornices loom over larger alpine objectives. Surface hoar growth has been observed in the alpine. Steep solar slopes have a thin sun crust. Low density snow (good skiing) persists in sheltered areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Significant wind effect exists in all alpine areas with isolated wind slabs in steep lee areas of the high alpine. Soft surface snow remains just below ridge crests at treeline. The upper snowpack is faceting and this has diminished the sensitivity of wind slabs and rendered the four layers of surface hoar that exist in the upper snowpack dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-5 cm new snow sits over 10-20 cm of surface facets at tree-line and below elevations and wind effected snow in alpine. The mid-pack is generally well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests and ski cutting.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Surface faceting continues with cooler temperatures. Previous winds have stripped snow from all exposed terrain creating hard wind slabs and wind affected snow in any open terrain. The mid-pack is supportive. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Little change, other than continued facetting and softening of previous wind effect from extreme southerly winds. Cold-weakened cornices loom over larger alpine objectives. Surface hoar growth has been observed in the alpine. Steep solar slopes, tilted S-SW, have a thin sun crust. Low density snow (good skiing) persists in sheltered areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">2-5 cm new snow sits over 10-20 cm of surface facets at tree-line and below elevations and wind effected snow in alpine. The mid-pack is generally well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests and ski cutting.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15+ cm new snow with the most in the southern areas. The new snow sits over 10-20 cm of facets at tree-line and below and over previous wind effect in the alpine. The mid-pack is generally well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests. The Nov crust/facets are near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Alpine is either stripped of snow completely or offers a variety of wind affected surfaces. Surface faceting continues with cooler temperatures. Strong mid-pack overlies generally supportive basal layers. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations, in the very southern parts of the park. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few cm of new snow covers a mixture of surface facets, old wind affected snow, sun crusts and surface hoar. Ski pen is up to 25cm in sheltered areas. The snowpack is predominantly made up of strong rounded crystals. Critical layers from earlier in the winter are dormant for now.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">5cm of snow on wed night has been redistributed by Moderate SW wind. Reactive wind slabs may be found in isolated lee areas in the alpine. A crust exists below 1900m that varies from bulletproof to breakable dependent on aspect and elevation. Areas east of the divide hold a thinner &amp; more faceted snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15+ cm new snow with the most in the southern areas. The new snow sits over 10-20 cm of facets at tree-line and below and over previous wind effect in the alpine. The mid-pack is generally well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests. The Nov crust/facets are near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-40 cm of storm snow with the most in the southern areas. The storm snow sits over facets in sheltered areas and over previous wind effect in exposed alpine and tree line areas. The mid-pack is well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests. The Nov crust/facets are near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Alpine is either stripped of snow completely or offers a variety of wind affected surfaces. Surface faceting continues with cooler temperatures. Strong mid-pack overlies generally supportive basal layers. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations, in the very southern parts of the park. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 cm of new snow covers a mixture of surface facets, old wind affected snow, sun crusts and surface hoar. Ski pen is up to 35cm in sheltered areas. The snowpack is predominantly made up of strong rounded crystals. Critical layers from earlier in the winter are dormant for now.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of storm snow with the most in the southern areas. The storm snow sits over facets in sheltered areas and over previous wind effect in exposed alpine and tree line areas. The mid-pack is well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-30 cm of storm snow with the most in the southern areas. The storm snow sits over facets in sheltered areas and over previous wind effect in exposed alpine and tree line areas. The mid-pack is well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests. The Nov crust/facets are near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Alpine is either stripped of snow completely or offers a variety of wind affected surfaces. Surface faceting continues with cooler temperatures. Strong mid-pack overlies generally supportive basal layers. Decomposing surface hoar is found down 40cm to 80cm in isolated sheltered locations, in the very southern parts of the park. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10 cm of new snow has not yet built much of a slab over the previous drought layer (surface facets, surface hoar, wind affect, and sun crust). Ski pen of up to 35cm in sheltered area means sluff management is still key in steep terrain. The snowpack below is mostly strong rounded crystals, with critical layers from earlier this winter now dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-30 cm of storm snow with the most in the southern areas. The storm snow sits over facets in sheltered areas and over previous wind effect in exposed alpine and tree line areas. The mid-pack is well settled with the various persistent weak layers visible in the snowpack but unreactive to stability tests. The Nov crust/facets are near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15cm of snow in the past 24hrs brings the storm total to 15-40cm, with the most in the southern part of the region. The storm snow sits over facets in sheltered areas and over previous wind effect in exposed alpine and tree line areas. The mid-pack is well settled and unreactive to stability tests. The Nov crust/facets are near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 35cm of storm snow could accumulate up to Mon eve. Expect to find new wind slab on lee ridgetop features and below. The new snow will overlie previously wind affected surfaces in non-sheltered areas in the alpine and below as well as widespread surface facets. Strong mid-pack in deeper areas overlies supportive basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow (15-20cm so far) is beginning to build a slab over the previous drought layer (surface facets, surface hoar, wind affect, and sun crust).  As the wind picks up and snowfall continues, expect reactive storm slabs to develop quickly. The snowpack below is mostly well bonded, with critical layers from earlier this winter now dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-15cm of snow in the past 24hrs brings the storm total to 15-40cm, with the most in the southern part of the region. The storm snow sits over facets in sheltered areas and over previous wind effect in exposed alpine and tree line areas. The mid-pack is well settled and unreactive to stability tests. The Nov crust/facets are near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 40cm of storm snow has fallen at the higher elevations by Tuesday. This snow is deep and low density below treeline and is forming slabs up to 100 cm deep at treeline and alpine areas where the wind is doing some light drifting. Watch for any slab formation in the new snow and dry loose avalanches running easily in gullies and steep terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to a total of 30cm of storm snow accumulated by Tuesday morning. Expect to find new wind slab on lee ridge-top features and below. The new snow will overlie previously wind affected surfaces in non-sheltered areas in the alpine and below as well as widespread surface facets. Strong mid-pack in deeper areas overlies supportive basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A heavy, 20cm storm slab sits atop the previous drought layer (surface facets, surface hoar, wind affect, and sun crust). In wind-affected areas, expect reactive storm slabs. Pay close attention to cracking/whumphing around your skis and in lee areas. The snowpack below is mostly well bonded, with critical layers from earlier this winter dormant.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">10-25 cm of snow is expected at higher elevations tuesday. Rapid loading during tuesdays storm will form storm slabs over top of old wind slab. Previous wind slab sits on a firm crust below 1900m.  We have not found the buried surface hoar that has been causing instability in neighboring regions but this problem may still exist in isolated pockets. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 40cm of storm snow has fallen at the higher elevations by Tuesday. This snow is deep and low density below treeline and is forming slabs up to 100 cm deep at treeline and alpine areas where the wind is doing some light drifting. Watch for any slab formation in the new snow and dry loose avalanches running easily in gullies and steep terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 10-20 cm of new snow on Tuesday brings totals to 30-60 cm since Jan. 27th. This snow is low density below treeline, but is forming slabs up to 100 cm deep above treeline where the wind is doing some light drifting. The lower snowpack has a series of persistent weak layers that remain dormant. Snowpack amounts at treeline are 150-220 cm</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Storm total of 30cm accumulated in the Icefields region. New snow over a mixed, facet interface to a strong mid-pack. Bond at the storm interface showing mixed results through the forecast region. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A heavy, 40-50cm storm slab sits atop the previous drought layer (surface facets, surface hoar, wind affect, and sun crust). Overnight winds are rapidly building these into touchy slabs at all elevations. Previously dormant layers deeper in the snowpack (surface hoar/crust) may be waking up with the sudden heavy burden.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 15cm of new snow is expected at higher elevations tuesday. Tuesdays storm will form storm slabs over top of old wind slab. Previous wind slab sits on a firm crust below 1900m. We have not found the buried surface hoar that has been causing instability in neighboring regions but this problem may still exist in isolated pockets. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 10-20 cm of new snow on Tuesday brings totals to 30-60 cm since Jan. 27th. This snow is low density below treeline, but is forming slabs up to 100 cm deep above treeline where the wind is doing some light drifting. The lower snowpack has a series of persistent weak layers that remain dormant. Snowpack amounts at treeline are 150-220 cm</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60 cm of snow over the last week. This snow is low density below tree line, but is forming slabs up to 100 cm deep above tree line where the wind has redistributed it in lee features. The mid snowpack has a series of persistent weak layers that remain dormant. Height of snow at tree line is 150-220 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">40-60cm of new storm snow appears to be bonding well to the old surface, on a mixed form/facet interface giving hard, sudden planar results in field tests at the Icefields. Soft-slab will continue to develop on all aspects and elevations as the snow settles. Mid-pack remains strong underfoot except in areas where the snowpack is less than 100cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Another 15cm last night, brings our storm total to ~80cm at TL, with the bulk of the precip falling on Monday and Tuesday. The brunt of the storm brought warm temperatures, and strong winds creating touchy storm slabs. The new snow buries a previous drought layer (surface facets, surface hoar, wind affect, and sun crust).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-60 cm of snow over the last week. This snow is low density below tree line, but is forming slabs up to 100 cm deep above tree line where the wind has redistributed it in lee features. The mid snowpack has a series of persistent weak layers that remain dormant. Height of snow at tree line is 150-220 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong Westerly winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. The mid snowpack has a series of persistent weak layers that remain dormant. Height of snow at tree line is 150-220 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">40-60cm with minimal wind effect. This new snow overlies surface facetting, previous wind effect and surface hoar depending on location.  Well settled mid-pack characteristic for the region except in typical shallow locations. Variable HS (90-200cm) throughout the area.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">An accumulated 60+ cm of storm snow from earlier this week buries Surface Hoar, Crusts, and or Facets depending on elevation and aspect. Storm slabs remain reactive in the Alpine and exposed areas of TL. Persistent slabs are still being triggered yesterday at and below TL. Our mid and lower snowpack is quite strong, with no current concerns.&nbsp; </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Southwest wind has redistributed recent snowfall scouring westerly alpine start zones and creating wind slab on lee and cross loaded slopes. Fresh wind slab sits on a firm crust below 1900m. The mid snowpack is well consolidated at Cameron Lake but the snowpack becomes shallow and faceted in areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong Westerly winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. The mid snowpack has a series of persistent weak layers that remain dormant. Height of snow at tree line is 150-220 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong Westerly winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. The mid snowpack has a series of persistent weak layers that remain dormant. Height of snow at tree line is 150-220 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent HST (40-60cm) is forming wind slabs in the alpine and exposed tree line. This new snow overlies previous surface facetting, surface hoar and wind affected snow depending on the location. A well settled mid-pack, except in areas with a shallow snowpack, can be found throughout the forecast region. Variable HS (90-200cm) throughout the area.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm slabs continue to receive new inputs in the form of fresh snow and wind. 60+ cm of storm snow from earlier this week sits on Surface Hoar, Crusts, and or Facets depending on elevation and aspect, on what is being called the January 24th persistent weak layer. The mid and lower snowpack is quite strong, with no current concerns. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Southwest through northeast wind has redistributed 10-15cm recent storm snow creating wind slab on lee and cross loaded slopes. Fresh wind slab sits on a firm crust below 1900m. The mid snowpack is well consolidated at Cameron Lake but the snowpack becomes shallow and faceted in areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong Westerly winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. The mid snowpack has a series of persistent weak layers that remain dormant. Height of snow at tree line is 150-220 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Cold temps promoting surface facetting. HST (25-55cm) bonding well to underlying surfaces (facets, surface hoar and wind affected snow depending on location). Wind slabs in the ALP and exposed TL. A well settled mid-pack, except in areas with a shallow snowpack, can be found throughout the forecast region. Variable HS (90-200cm).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong winds combined with recent storm snow created isolated wind slabs and deep loading in alpine and exposed treeline areas. The January 26th persistent week layer is buried 60-80cm and consists of decomposing surface hoar in sheltered areas and a thin crust on solar aspects. The mid and lower snowpack is quite strong, with no current concerns. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Treeline snow depths range from 220-260cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Cold temperatures promoting surface facetting. HST (25-55cm) bonding well to underlying surfaces (facets, surface hoar and wind affected snow depending on location). Wind slabs in the ALP and exposed TL. A well settled mid-pack, except in areas with a shallow snowpack, can be found throughout the forecast region. Variable HS (90-200cm).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snow from the Feb 2 storm has been redistributed by strong south winds, followed by a switch to northwesterlies in some locations. The Jan 26 persistent weak layer is buried 60-80cm and consists of decomposing surface hoar in sheltered areas and a thin crust on solar aspects. The mid and lower snowpacks are strong, with no current concerns. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">30-35cm of new fluffy snow has fallen at Cameron Lake with limited wind effect at treeline and below. In the alpine, new snow has been distributed by westerly winds. New snow sits over previous wind slab which overlies a crust below 1900m. The midpack is well consolidated at Cameron Lake but quickly becomes faceted in areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Cold temperatures are promoting surface facetting. Previous HST (25-55cm) is bonding well to underlying surfaces (facets, surface hoar, wind affected snow depending on location). Wind slabs in the ALP and exposed TL. A well settled mid-pack, except in shallow snowpack areas, can be found throughout the forecast region. Variable HS (90-200cm).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snow from the Feb 2 storm was redistributed by strong S winds, then switched to NW'ly. Isolated pockets of soft slab can be found at ridge-top lee areas. Cold temps are beginning to lock this layer in. The Jan 26 persistent weak layer is buried 60-80cm and consists of decomposing surface hoar in sheltered areas and a thin crust on solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold has deeply penetrated the snowpack, promoting profound facetting in the upper 40cm. This will slow any slab development on the recent storm snow. The mid-pack has remained strong but, will loose strength over time with the prolonged arctic influence, especially where shallow.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow from last week was redistributed by strong S'ly, then NW'ly, winds. These wind slabs are beginning to facet and weaken, but are still popping out on unsupported features at higher elevations. The Jan 26 persistent weak layer (surface hoar and/or thin crust) is buried 60-80cm but has not seen activity in the last few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">30-35cm of fluffy snow sits on the surface at Cameron Lake with limited wind effect at treeline and below. In the alpine, new snow has been distributed by westerly winds. New snow sits over previous wind slab which overlies a crust below 1900m. The midpack is well consolidated at Cameron Lake but quickly becomes faceted in areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine and exposed areas at tree line. In sheltered areas the recent storm snow remains loose powder. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have redistributed the recent 30-60cm of low density storm snow into wind slab in the alpine. In sheltered areas, the latest storm snow remains somewhat low density. Buried sun crust and facets on steep south aspects. Treeline snow depths range from 150-220cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold has deeply penetrated the snowpack, promoting profound facetting in the upper 40cm. This will slow any slab development on the recent storm snow. The mid-pack has remained strong but, will loose strength over time with the prolonged arctic influence, especially where shallow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm snow from last week was redistributed by strong S'ly, then NW'ly, winds. These wind slabs are beginning to facet and weaken, but are still popping out on unsupported features at higher elevations. Loose, dry sluffs are traveling fast and far in steep alpine gullies. Cornices are rotting at their bases due to the cold temps and may be fragile.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have created wind slabs in lee areas of the alpine, and wind effect in many open alpine and treeline areas. In sheltered areas the surface snow is facetting quickly and beginning to sluff more easily in steep terrain. A buried thin sun crust and facet layer from Jan 27th is present on steep south aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold continues to promote rapid facetting in the upper 40cm. This is slowing slab development within the the recent Feb 3rd 40cm of storm surface snow. The mid-pack has remained strong and supportive but is showing signs of loosing strength with the prolonged arctic influence, especially where it is shallow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous strong S'ly, then NW'ly, winds built slabs in exposed areas, these are facetting and softening, but remain reactive in isolated pockets. Facetting of surface snow is also making loose dry avalanches possible in steep terrain.  A weak interface of a suncrust with facets, surface hoar was buried in late January and is now down 70-90cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">35cm of powder snow sits on the surface at Cameron Lake with limited wind effect at treeline &amp; below. Low density snow has been redistributed by NW-NE winds creating soft windslab in the alpine &amp; near ridgetop. Recent snow sits on previous windslab which overlies a crust below 1900m. Midpack is well consolidated but becomes faceted in shallow areas</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have created wind slabs in lee areas of the alpine, and wind effect in many open alpine and treeline areas. In sheltered areas the surface snow is facetting quickly and beginning to sluff more easily in steep terrain. A buried thin sun crust and facet layer from Jan 27th is present on steep south aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have created wind slabs in lee areas of the alpine, and wind effect in many open alpine and treeline areas. In sheltered areas the surface snow is facetting quickly and beginning to sluff more easily in steep terrain. A buried thin sun crust and facet layer from Jan 27th is present on steep south aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold weather continues to promote facetting of the upper 40cm. The mid-pack has remained strong and supportive, but is showing signs of loosing strength with the prolonged arctic influence, especially where it is shallow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Renewed Northerly winds have added to previously formed slabs in exposed areas, these are facetting quickly, but remain reactive in lees. Facetting of surface snow is also making sluffs possible in steep terrain. A weak interface of a suncrust with facets and surface hoar, was buried in late January and is now down 60-100cm. Cornices are weakening.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Previous winds from all directions have created wind slabs in some lee areas of the alpine, and wind effect in many open alpine and treeline areas. In sheltered areas the surface snow is facetting quickly and beginning to sluff more easily in steep terrain. A buried thin sun crust and facet layer from Jan 27th is present on steep south aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Winds have created small slabs in lee areas of the alpine, and wind effect in open alpine and treeline areas. The surface snow is facetting quickly and beginning to sluff more easily in steep terrain. A facet layer from Jan 27th is present at treeline and in the alpine down 30-40cm. On steep south this layer may consist of a thin sun crust as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold weather continues to promote facetting of the upper 40cm. The mid-pack is showing signs of losing strength with the prolonged arctic influence, especially where it is shallow. Widespread wind effect in the alpine and upper tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold has been weakening cornices and the upper snowpack. Widespread wind effect in the alpine has made for variable travel. The January weak interface down 70-100 is reducing in strength with increasing facetting. The mid and lower snowpack are still relatively strong having rounded under previous mild temperatures and snow load.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Winds have created small slabs in lee areas of the alpine, and wind effect in open alpine and treeline areas. The surface snow is facetting quickly and beginning to sluff more easily in steep terrain. A facet layer from Jan 27th is present at treeline and in the alpine down 30-40cm. On steep south this layer may consist of a thin sun crust as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Winds have created small slabs in lee areas of the alpine, and wind effect into open areas at treeline. The surface snow is facetting and beginning to sluff more easily in steep terrain. A facet layer from Jan 27th is present at treeline and in the alpine down 30-40cm. On steep south this layer may consist of a thin sun crust as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold weather continues to promote facetting of the upper 40cm. The mid-pack is showing signs of losing strength with the prolonged arctic influence, especially where it is shallow. Widespread wind effect in the alpine and upper tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold has weakened cornices and the upper snowpack. Widespread wind effect in the alpine has made for variable travel. The January weak interface down 70-100 is reducing in strength with facetting due to the cold. The mid and lower snowpack are still relatively strong having rounded under previous mild temperatures and snow load.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Variable winds have created small slabs in the alpine, and wind effect in open areas at treeline. The surface snow is faceting and beginning to sluff more easily in steep terrain. A facet layer from Jan 27th down 30-40 cm is of note especially near treeline. On steep south slopes this layer may also involve a thin crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated small wind slabs exist in exposed alpine and treeline areas. In sheltered areas, the surface snow is facetted and is starting to sluff more easily in steep terrain. A facet layer from Jan 27th is present at treeline and in the alpine down 30-40. On steep south this layer may consist of a thin sun crust as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The upper snowpack has facetted from the recent cold temperatures and overlies a supportive mid-pack, except in shallow areas where the entire snowpack is weak and facetted. Variable wind effect in the alpine and at tree line.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The cold has weakened cornices and the upper snowpack. Widespread wind effect in the alpine has made for variable travel. The January 24th weak interface down 70-100 is reducing in strength with facetting due to the cold. The mid and lower snowpack are still relatively strong having rounded under previous mild temperatures and snow load.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> Last weeks snow is settling well in sheltered areas at Cameron Lake but pockets of wind slab continue to develop in unusual places due to variable wind direction. Surface snow sits over old wind slab which overlies a melt freeze crust below 1900m. Mid snowpack is well consolidated but becomes faceted and shallow east of the Cameron Lake area. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated small wind slabs exist in exposed alpine and treeline areas. In sheltered areas, the surface snow is facetted and is starting to sluff more easily in steep terrain. A facet layer from Jan 27th is present at treeline and in the alpine down 30-40. On steep south this layer may consist of a thin sun crust as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind effect in the alpine with small isolated wind slabs. In sheltered areas, the surface snow is facetted and is sluffing more easily in steep terrain (40 degree). A facet layer from Jan 27th is present at treeline and in the alpine down 30-40. On steep south this layer may consist of a thin sun crust as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong SW winds and higher humidity are likely creating wind slabs in the alpine on lee features. The upper snowpack has facetted from the recent cold temperatures and overlies a supportive mid-pack, except in shallow areas where the entire snowpack is weak and facetted. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread wind effect in the alpine has made for tricky travel. Large lenses of dense, hard slab are mixed with cold, cream cheese powder. The cold has weakened cornices and the upper snowpack. The January 24th weak interface, down 70-100cm, is faceting and weakening in the cold. The mid-lower snowpack is still relatively strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Last weeks snow is settling well in sheltered areas at Cameron Lake but pockets of wind slab continue to develop in unusual places due to variable wind direction. Surface snow sits over old wind slab which overlies a melt freeze crust below 1900m. Mid snowpack is well consolidated but becomes faceted and shallow east of the Cameron Lake area. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wind effect in the alpine with small isolated wind slabs. In sheltered areas, the surface snow is facetted and is sluffing more easily in steep terrain (40 degree). A facet layer from Jan 27th is present at treeline and in the alpine down 30-40. On steep south this layer may consist of a thin sun crust as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated, thin windslabs persist in the high alpine and continued to form on Wednesday with most alpine snow surfaces being wind effected. At treeline and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong SW winds and higher humidity continue to create wind slabs in high alpine lee features. The upper snowpack has facetted from the recent cold temperatures and overlies a supportive mid-pack, except in shallow areas where the entire snowpack is weak and facetted. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of new snow covers a variety of old surfaces, from hard wind slabs in the alpine and exposed areas of TL, to low density facetted snow in sheltered areas at TL and below. The cold has weakened cornices and the upper snowpack. The January 24th interface is down 70-100cm and unreactive in stability tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated, thin windslabs persist in the high alpine and continued to form on Wednesday with most alpine snow surfaces being wind effected. At treeline and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect and isolated, thin wind-slabs throughout the alpine. At tree-line and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine winds continue to create wind slabs in high alpine lee features particularly where local terrain increases the wind action. The upper snowpack are facets and mixed forms over a supportive mid-pack. Thinner snowpack areas it is weak, un-supportive, and facetted. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Approx 15cm of new snow covers a variety of old surfaces, from hard wind slabs in the alpine and exposed areas of TL, to low density facetted snow in sheltered areas at TL and below. Cold temps continue to facet the upper snowpack, and weaken cornices. The January 24th interface is down 70-100cm and predominantly unreactive in stability tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Southwest winds have returned building wind slabs which sit over a layer of facets. Facet layer has developed over a variety of hard surfaces including old wind slab and a deteriorating melt freeze crust below 1900m. Mid snowpack has become faceted, especially in shallow areas east of Cameron Lake. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect and isolated, thin wind-slabs throughout the alpine. At tree-line and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect and isolated, thin wind-slabs throughout the alpine. At tree-line and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Alpine winds have created wind slabs or hard surface conditions in high alpine lee features particularly where local terrain increases the wind action. The upper snowpack are facets and mixed forms over a supportive mid-pack. Thinner snowpack areas it is weak, un-supportive, and facetted. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20cm of snow in the last few days covers the cold weakened drought surface. Facets, wind effect and crusts lie under the new snow and make a poor interface for it to bond to. Surface hoar, crusts and facets have still been found down 70-100cm on the January 24th persistent interface. The mid and lower snowpack remain strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect and isolated, thin wind-slabs throughout the alpine. At tree-line and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect with a few thin wind-slabs and fresh cornice growth developing in the alpine. At treeline and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain although wind effect is starting to creep down. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong ridge top winds from the SW have created wind slabs or hard surface conditions in alpine and tree line features. In sheltered areas the top 30-60cm is faceted snow over a supportive mid-pack where the snowpack is deeper. Thin snowpack areas are weak, un-supportive, and facetted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15cm of snow overnight, brings the total to 20-40cm over the Feb. 14th drought interface; this is predominantly a wind crust in exposed areas near the height of the pass, and buried windslabs and facets as you move East and West. Facets, and a waek suncrust still linger down ~70cm at the Jan. 24th PWL. The mid and lower snowpack are strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect with a few thin wind-slabs and fresh cornice growth developing in the alpine. At treeline and below the snowpack is well settled except the surface snow which is facetted and sluffs in steep terrain although wind effect is starting to creep down. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong to extreme SW winds, warm temps and new snow are creating wind slabs and storm slabs over the old faceted surface. We suspect this new storm snow/facet interface to be reactive. Below the newly formed instabilities the Jan 27 facet / sun crust persistent layer exist at tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong ridge top winds from the SW have created wind slabs or hard surface conditions in alpine and tree line features. In sheltered areas the top 30-60cm is faceted snow over a supportive mid-pack where the snowpack is deeper. Thin snowpack areas are weak, un-supportive, and facetted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong south winds and up to 10cm of snow overnight. The Feb 14 drought interface is now down 30-50cm in sheltered areas; this interface is predominantly a wind crust in exposed areas near the height of the pass, and buried windslabs and facets as you move East and West. Facets, and a weak suncrust still linger down ~80cm at the Jan. 24th PWL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Extreme southwest through westerly winds continue to build wind slabs over a weak facet layer on top of older facetted snow. In lower elevations, this sits on a hard crust increasing the potential for wide propagations. Midpack is made up of facets and decomposing crusts of varying resistance. Thin snowpack areas are very facetted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive wind effect and isolated, thin wind-slabs throughout the alpine from extreme wind on Sunday. Approximately 40cm of recent storm snow is present at tree line tapering down to 15cm below tree line. A facet and sun crust layer buried Jan 27 persists at treeline down 30-40 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-50 cm of storm snow over the last three days along with strong to extreme west winds has created windslabs in exposed alpine and treeline areas. This sits on top of either old wind effect in areas that were previously wind effected or soft facets in previously sheltered areas. The Jan. 27th interface of facets/sun crust is now down 30-70 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong ridge top winds from the SW have created wind slabs or hard surface conditions in alpine and tree line features. In sheltered areas the top 30-60cm is faceted snow over a supportive mid-pack where the snowpack is deeper. Thin snowpack areas are weak, un-supportive, and facetted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extreme south winds and a warm 40mm of precip overnight. The Feb 14 drought interface is now down 50-70cm in sheltered areas; this interface is predominantly a wind crust in exposed areas near the height of the pass, and buried windslabs and facets as you move East and West. Facets and a weak suncrust still linger down 80-100cm on the Jan 24th PWL. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30-50 cm of storm snow over the last three days along with strong to extreme west winds has created windslabs in exposed alpine and treeline areas. This sits on top of either old wind effect in areas that were previously wind effected or soft facets in previously sheltered areas. The Jan. 27th interface of facets/sun crust is now down 50-90 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm deposited between 30-40 cm of new snow along with very strong winds and warming temperatures to create widespread storm slabs failing on the Fe 19 facets layer underlying. Expect this snowpack to remain very sensitive to human triggering for the next few days as the snowpack slowly begins settle.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Moderate to strong ridge top winds from the SW have created wind slabs or hard surface conditions in alpine and tree line features. In sheltered areas the top 30-60cm is faceted snow over a supportive mid-pack where the snowpack is deeper. Thin snowpack areas are weak, un-supportive, and facetted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">80mm of precip in the last 3 days, extreme S'ly winds, and mild temps have created a widespread surface storm slab. Thickness of the new slab will vary from 50-100cm. This sits on the Feb 14 drought interface, which is predominantly a wind crust in exposed areas near the height of the pass, and buried windslabs and facets as you move East and West. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The recent storm deposited between 30-40 cm of new snow along with very strong winds and warming temperatures to create widespread storm slabs failing on the Fe 19 facets layer underlying. Expect this snowpack to remain very sensitive to human triggering for the next few days as the snowpack slowly begins settle.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The last storm stared with extreme winds then deposited 50cm of snow creating a widespread avalanche cycle failing mainly below this storm snow. Indications are that the surface snow needs some wind in order to stiffen the slab, otherwise it won't propagate. Settlement will be slow over the next few days and this slab will release with triggers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Mod to Strong ridge top winds from the SW have created wind slabs or hard surface conditions in Alp &amp; TL. Wind slabs overlie facets which will bond poorly. In sheltered areas the top 30-60cm is faceted snow over a supportive mid-pack where the snowpack is deeper. Thin snowpack areas are weak, un-supportive, and facetted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The 80mm of precip earlier in the week, extreme S'ly winds, and mild temps have created a widespread persistent slab. This sits on the Feb 14 drought interface, which is a wind crust in exposed areas near Rogers Pass, and buried windslabs/facets as you move East or West. This new slab is of most concern in wind-exposed areas in the Alpine and TL.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The last storm stared with extreme winds then deposited 50cm of snow creating a widespread avalanche cycle failing mainly below this storm snow. Indications are that the surface snow needs some wind in order to stiffen the slab, otherwise it won't propagate. Settlement will be slow over the next few days and this slab will release with triggers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 to 10cm of new snow arrived with strong winds Thursday contributing to the wind slabs above the February 19 interface created by 50cm of snow combined with extreme west winds over the weekend. Now down 60 to 90cm,  facets buried Jan 27 provide weak support for the upper snowpack and have been entrained as avalanches gouge down to them.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Varied depth wind slabs or hard surface conditions in Alp &amp; TL. Slabs overlie a facet interface down as much as 20 to 40cm, with varied and questionable bonding strength. Sheltered areas, top 30-60cm is faceted snow over a mostly supportive mid-pack. Reminder to be cautious of thick to thin characteristics, especially on a the surface slab.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow (15cm and counting) is covering settled storm snow, and a thin suncrust on steep solar aspects. The 80mm of precip, and extreme S'ly winds from earlier in the week sits on the Feb 14 drought interface (a wind crust in exposed areas near Rogers Pass, and buried windslabs/facets as you move East or West). </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Extreme SW-W winds have hammered the snowpack, distributing up to 40cm of recent storm snow and forming slabs. These sit on the weak February 14 facet layer which is above a melt freeze crust at treeline and below. The remainder of the midpack is made up of dense facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 to 10cm of new snow arrived with strong winds Thursday contributing to the wind slabs above the February 19 interface created by 50cm of snow combined with extreme west winds over the weekend. Now down 60 to 90cm, facets buried Jan 27 provide weak support for the upper snowpack and have been entrained as avalanches gouge down to them.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 15 cm of new snow on Friday. Recent snow and wind have created wind slabs in alpine lee areas and exposed treeline slopes. In thin snowpack areas the recent 30-50 cm of storm snow sits over weaker facet interfaces which fail more easily in tests. In deeper snowpack areas there was less facetting, and the recent storm snow is bonding better.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread extensive wind effect in the alpine and is highly variable. The lee has windslabs (generally hard) that are well down into the terrain. The windward has been heavily stripped. Treeline and below has wind effect in any exposed terrain. The snowpack below the alpine is faceted with depth hoar near the base and is failing in test results.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow (up to 45cm) has formed fresh storm slabs over previously settled storm snow, and a thin suncrust on steep solar aspects. The 80mm of precip, and extreme S'ly winds from early in the week sit on the Feb 14 drought interface; a wind crust in exposed areas near the Pass; buried windslabs, facets, and a thin suncrust as you move East or West. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Extreme SW-W winds have hammered the snowpack, distributing up to 40cm of recent storm snow and forming slabs. These sit on the weak February 14 facet layer which is above a melt freeze crust at treeline and below. The remainder of the midpack is made up of dense facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over a meter of new snow has fallen at treeline in the Little Yoho region over the last week with recent winds creating wind slabs in alpine and exposed treeline lee areas. The new snow has settled into 50-80 cm of storm snow over the Feb 19 interface and seems to be bonding well in most places. Surface snow is sluffing easily in steep terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30cm of storm snow since Friday. Snow and wind have created wind slabs in alpine lee areas and exposed treeline slopes. In thin snowpack areas 30-60 cm of snow sits over weak facet interfaces which fail more easily in tests. In deeper snowpack areas there was less facetting, and the recent storm snow is bonding better. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread extensive wind effect in the alpine and is highly variable. The lee has windslabs (generally hard) that are well down into the terrain. The windward has been heavily stripped. Treeline and below has wind effect in any exposed terrain. The snowpack below the alpine is faceted with depth hoar near the base and is failing in test results. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow (up to 55cm) has formed fresh storm slabs over previously settled storm snow, and a thin suncrust on steep solar aspects. The 80mm of precip, and extreme S'ly winds from early in the week sit on the Feb 14 drought interface; a wind crust in exposed areas near the Pass; buried windslabs, facets, and a thin suncrust as you move East or West. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over a meter of new snow has fallen at treeline in the Little Yoho region over the last week with recent winds creating wind slabs in alpine and exposed treeline lee areas. The new snow has settled into 50-80 cm of storm snow over the Feb 19 interface and seems to be bonding well in most places. Surface snow is sluffing easily in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30cm of storm snow since Friday. Snow and wind have created wind slabs in alpine lee areas and exposed tree line slopes. In thin snowpack areas 30-60 cm of snow sits over weak facet interfaces and facet sun crust interfaces on southerly aspects. In deeper snowpack areas there was less facetting, and the recent storm snow is bonding better. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread wind effect in open areas at all elevations. Leeward features have wind slabs that are well down into the terrain, and windward aspects have been heavily stripped. The snowpack below the alpine is faceted with depth hoar near the base and is failing in test results. </span></p>
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</style><p class="p_CC664AAA"><span class="s_F6B3DCA5">More snow has fallen on the west end of the park than east. Since Wednesday, up to 70cm has been redistributed by sustained moderate S'ly wind.  The Feb 14 drought interface is down ~1m in sheltered areas; this interface exists as a wind crust in exposed areas near the Pass, and buried windslabs, facets, or a thin suncrust as you move East or West.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over a meter of new snow has fallen at tree line in the Little Yoho region over the last week with recent winds creating wind slabs in alpine and exposed treeline lee areas. The new snow has settled into 50-80 cm of storm snow over the Feb 19 interface and seems to be bonding well in most places. Surface snow is sluffing easily in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds for the past 36-hours has blown the recent storm snow into windslabs in alpine lee areas and exposed tree line slopes. In Kootenay and around Lake Louise we are tracking a </span><a href="https://www.avalanche.ca/?panel=mountain-information-network-submissions/f956af78-7a33-11eb-88d6-46433e5c3157" target="_blank"><span class="s_9255B882">persistent layer of suncrust and facets down 30-60</span></a><span class="s_AA239A9B"> cm that is producing avalanches and test results. Heads up, this layer is isolated but reacts to skiers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued widespread wind effect in open areas at all elevations. Windward aspects have been heavily stripped of snow. The snowpack is highly variable. Shallow snowpack areas are weak and failing in compression tests, while the mid-pack is supportive in areas where the snowpack is deeper.</span></p>
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</style><p class="p_CC664AAA"><span class="s_F6B3DCA5">More snow has fallen on the west end of the park than east. Since Wednesday, up to 70cm has been redistributed by sustained moderate S'ly wind. The Feb 14 drought interface is down ~1m in sheltered areas; this interface exists as a wind crust in exposed areas near the Pass, and buried windslabs, facets, or a thin suncrust as you move East or West.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Strong SW wind has caused significant cornice growth and added to surface wind slab. 20-50cm wind slab sits on top of the weak February 14 facet layer which is above a melt freeze crust at treeline and below. The remainder of the midpack is made up of dense facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Windslabs and wind effect dominate the surface of the snowpack above 2000 m, but otherwise at treeline and below </span><a href="https://www.avalanche.ca/?panel=mountain-information-network-submissions/d4b3367c-7ae6-11eb-8c95-7ebe890cf52e" target="_blank"><span class="s_9255B882">the snowpack in Little Yoho is deep and strong with no obvious weak layers.</span></a><span class="s_AA239A9B"> The exception to this might be south aspects, where buried crusts may lurk and also the Mt Dennis area, where the snowpack is generally shallower.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds have blown the recent storm snow into windslabs in alpine lee areas and exposed tree line slopes. In Kootenay and around Lake Louise we are tracking two </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/473fd502-7baf-11eb-b9b7-d6f5b8c172ff" target="_blank"><span class="s_9255B882">persistent layers of facets and suncrust down 30-80</span></a><span class="s_AA239A9B"> cm that are producing avalanches and test results. Heads up, these layers are isolated but have been reactive to skiiers recently</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Continued widespread wind effect with some light precip. transported through open areas at all elevations. Windward aspects have been heavily stripped of snow, creating hard windslabs in all lee features. Highly variable snowpack across the region, with shallow areas failing at the faceted base, while deeper regions have a strong mid-pack bridge. </span></p>
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</style><p class="p_CC664AAA"><span class="s_F6B3DCA5">Extreme southerly winds overnight (up to 118km/h!) will have created a variety of new surface slabs in exposed areas. Below the fresh snow transport, the upper snowpack continues to settle and gain strength. The Feb 14 drought interface is down ~1m in sheltered areas; this interface exists as buried windslabs, facets, or a thin suncrust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds have blown the recent storm snow into windslabs in alpine lee areas and exposed tree line slopes. In Kootenay and around Lake Louise we are tracking two </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/473fd502-7baf-11eb-b9b7-d6f5b8c172ff" target="_blank"><span class="s_9255B882">persistent layers of facets and suncrust down 30-80</span></a><span class="s_AA239A9B"> cm that are producing avalanches and test results. Heads up, these layers are isolated but have been reactive to skiiers recently</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Strong SW winds have scoured exposed slopes and formed wind slab in alpine lee areas and open tree line slopes. In Kootenay and around Lake Louise we are tracking two </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/473fd502-7baf-11eb-b9b7-d6f5b8c172ff" target="_blank"><span class="s_9255B882">persistent layers of facets and sun crust down 30-80</span></a><span class="s_AA239A9B"> cm that are producing avalanches and sudden test results. These layers are isolated but have been reactive to skiers recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Snowpack morphing from cold/dry, to warm/moist spring conditions. Top 5-15cm moist snow over a supportive mid-pack  in the Icefields. Windward aspects have been heavily stripped of snow. Highly variable snowpack across the region, with shallow areas failing at the faceted base, while deeper regions have a strong bridge over a weak base. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Recent strong to extreme winds have left behind a variety of wind slabs in the Alpine and exposed areas of TL. In sheltered areas at and below TL the snowpack is generally &quot;right side up&quot; with decent riding conditions. The February drought layer is buried ~1m, and the Jan 24th layer is down ~1.4m; both layers have been unreactive in snowpack tests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Strong SW winds have scoured exposed slopes and formed wind slab in alpine lee areas and open tree line slopes.</span><span class="s_AA239A9B"> In the Little Yoho Valley, the height of snow at tree line is ~280cm and does not have the same Persistent Slab problem as Banff and Kootenay.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Top 5 cm moist snow on steep solar aspects and top 5-10 cm at treeline and below (except North aspects). Previous strong SW winds scoured alpine ridges and created windslab in many exposed areas.  These windslabs and two </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/473fd502-7baf-11eb-b9b7-d6f5b8c172ff" target="_blank"><span class="s_9255B882">persistent layers of facets and sun crust down 30-80</span></a><span class="s_AA239A9B">  cm are the sliding layers for avalanches to size 3 throughout the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warm temperature have resulted in warm moist conditions at TL and BTL. The snowpack is highly variable throughout the forecast region. A moist upper snowpack overlies a supportive mid-pack in the Icefields area. Shallow snowpack areas are week and failing in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Recent strong to extreme winds left behind a variety of wind slabs in the Alpine and exposed areas of TL. The surface snow turned moist yesterday at lower elev on all asp, and higher on solar asp. Strong solar input today will destabilize the upper snowpack again. The February facet layer is buried 80cm to 1+m, depending on asp &amp; elev.</span></p><p class="p_CC664AAA"><span class="s_1681A555"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Surface snow will quickly become moist as the sun beats down and freezing levels rise to ridge top. 20-50cm wind slab sits on top of the weak February 14 facet layer which is above a melt freeze crust at treeline and below. The remainder of the midpack is made up of dense facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Strong SW winds have scoured exposed slopes and formed wind slab in alpine lee areas and open tree line slopes.  Expect a new surface crust on solar aspects. </span><span class="s_AA239A9B"> In the Little Yoho Valley, the height of snow at tree line is ~280cm and does not seem to have the same Persistent Slab problem as Banff and Kootenay region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Its crust season. Expect these to be widespread at lower elevations. Previous strong SW winds scoured alpine ridges, creating wind slab in some alpine lees. 2 active persistent layers (Feb 19, Jan 27) of facets and /or suncrust are 30-80cm down on average. In thin areas, the basal depth hoar and crust is still a prominent layer in the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snowpack is highly variable throughout the forecast region. Warm temperatures have created thin crust on solar aspects at TL and BTL.&nbsp; Upper snowpack, either wind or sun affected, overlies a still relatively supportive mid-pack in the Icefields area. Shallow snowpack areas are weak and failing within various faceted layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Yesterday above freezing temperatures climbed to 2200m creating moist surface snow. A weak overnight refreeze created a thin crust on solar exposures in the alpine and all aspects below treeline. Wind slabs exist near ridges, and low density powder remains on high noth aspects. The February facet/ crust persistent weak layer is down 80-120cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Strong SW winds have scoured exposed slopes and formed wind slab in alpine lee areas and open tree line slopes. Expect a new surface crust on solar aspects and lower elevations.</span><span class="s_AA239A9B"> In the Little Yoho Valley, the height of snow at tree line is ~280cm and does not seem to have the same Persistent Slab problem as Banff and Kootenay region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15 cm of new snow sits over a crust on solar aspects. Previous strong SW winds scoured alpine ridges and created wind slab in some alpine lee areas. Two persistent facet layers (Feb 19 &amp; Jan 27) are down 30-80cm and still producing sudden shears in some locations. In thin areas the basal depth hoar/crust from Nov is still quite prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10cm of new snow at treeline. Warm temps and high solar input have created crusts and moist snow on solar aspects at TL and BTL. Continuing SW winds have extensively redistributed the snow pack at TL and ALP. The midpack is supportive in deep areas, but shallow snowpack areas are weak and failing in buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Temperatures have begun to drop. At treeline,15cm of new snow sits atop a breakable crust and 10cm of moist snow. Localized extreme winds associated with the passing of a cold front increased snow loading near ridges. The February facet/ crust persistent weak layer is down 80-120cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15 cm of new snow sits over a crust on solar aspects. Previous strong SW winds scoured alpine ridges and created wind slab in some alpine lee areas. Small facets are present down 70-100 cm but we are getting minimal to no results in snowpack tests and not seeing avalanche activity on these layers like we are in the Banff and Kootenay regions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15 cm of new snow sits over a crust on solar aspects. Moderate SW winds are transporting this new snow at treeline ridge crests and above. Two persistent facet layers (Feb 19 &amp; Jan 27) are down 30-80cm and still producing sudden shears in some locations. In thin areas the basal depth hoar/crust from Nov is still quite prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warm temps and high solar input have created crusts and moist snow on solar aspects at TL and below. Continuing SW winds have extensively redistributed the snow pack at TL and ALP. The mid pack is supportive in deep areas, but shallow snowpack areas are weak and failing on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">At treeline,15cm of new snow sits atop a breakable crust and 10cm of moist snow. Localized extreme winds associated with the passing of a cold front on Friday, increased snow loading near ridges. The February facet/ crust persistent weak layer is down 80-120cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-15 cm of new snow sits over a crust on solar aspects. Moderate SW winds are transporting this new snow at treeline ridge crests and above. Facets are present down 70-100 cm but we are getting minimal to no results in snowpack tests and not seeing avalanche activity on these layers like we are in the Banff and Kootenay regions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Since Friday, up to 30 cm of recent snow sits over solar crusts and wind effect in open areas. New solar crusts on isolated steep slopes formed on Monday. Two persistent facet layers (Feb 19 &amp; Jan 27) are down 30-80cm and still producing sudden shears in some locations. In thin areas the basal depth hoar/crust from Nov is still quite prominent</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warm temps and high solar input have created crusts and moist snow on solar aspects at TL and below. Continuing SW winds have extensively redistributed the snow pack at TL and ALP. The mid pack is supportive in deep areas, but shallow snowpack areas are weak and failing on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Up to 30cm of new snow sits atop a breakable crust and moist upper layers of snow up to treeline, and old wind affect in the alpine. The February facet/ crust persistent weak layer is down 80-120cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A crust exists on the surface to ridgetop on solar aspects and at low elevations. This tops 20-50cm dense settled snow on top of the February 14 facet layer which is above a melt freeze crust at treeline and below. The remainder of the midpack is made up of dense facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Since Friday, up to 30 cm of recent snow sits over solar crusts and wind effect in open areas. New solar crusts on isolated steep slopes formed on Monday. Facets are present down 70-100 cm but we are getting minimal to no results in snowpack tests and not seeing avalanche activity on these layers like we are in the Banff and Kootenay regions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Since Friday, up to 30 cm of recent snow sits over solar crusts and wind effect in open areas. New solar crusts on low elevation steep slopes formed on Tuesday. 2 persistent facet layers (Feb 19 &amp; Jan 27) are down 30-80cm and still producing sudden shears in some locations. In thin areas the basal depth hoar/crust from Nov is still quite prominent.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High solar input have created crusts and moist snow on solar aspects at TL and below. Continuing SW winds have extensively redistributed the snow pack at TL and ALP. The mid pack is supportive in deep areas, but shallow snowpack areas are weak and failing on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">N'ly aspects are holding cold, dry snow with isolated wind slabs in immediate lee areas. Meanwhile, the March sun has enough punch to quickly moisten surface snow on S'ly aspects well into the alpine, causing moist/wet conditions. This also creates a breakable crust once the sun leaves the slope. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Since Friday, up to 30 cm of recent snow sits over solar crusts and wind effect in open areas. Facets are present down 70-100 cm but we are getting minimal to no results in snowpack tests and not seeing avalanche activity on these layers like we are in the Banff and Kootenay regions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Fresh snow in spotty areas from spring squalls, but mostly firm surface crust on south aspects up to at least 2600 m with softer snow found on north aspects. Minimal recent wind effect at higher elevations except in steep, alpine gullies. Profile at 2200 m today showed the Feb. 19 and Jan. 27 facets in the upper meter but no results on column test. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High solar input have created crusts and moist snow on solar aspects at TL and below. Continuing SW winds have extensively redistributed the snow pack at TL and ALP. The mid pack is supportive in deep areas, but shallow snowpack areas are weak and failing on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A dusting overnight (~5cm) has covered up a breakable suncrust on SE through W aspects, while N'ly aspects remain soft and dry. Yesterday's afternoon winds created isolated wind slabs in immediate lee areas and ridge crests.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Fresh snow in spotty areas from spring squalls, but mostly firm surface crust on south aspects up to at least 2600 m with softer snow found on north aspects. Minimal recent wind effect at higher elevations except in steep, alpine gullies. Profile at 2200 m today showed the Feb. 19 and Jan. 27 facets in the upper meter but no results on column test. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm recent snow lies over firm surface crust on south aspects up to at least 2600 m and settled snow on north aspects. Some recent wind effect at higher elevations that seems limited to ridge crests. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. Cornices are huge.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High solar input have created crusts and moist snow on solar aspects at TL and below. Expect this condition to increase in elevation with rising freezing levels. SW winds have redistributed the snow pack at TL and ALP. The mid pack is supportive in deep areas but weak in shallow areas where it fails on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">5cm new snow Wednesday night brings the total to 20cm in the last 3 days and 48cm since Saturday. A breakable suncrust can be found down 15cm in open areas and a second crust down 25cm on all aspects to treeline, higher on solar aspects</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A crust exists on the surface to ridgetop on solar aspects and at low elevations breaking down during the day. This tops 30-50cm dense snow above of the Feb 14 facet layer which is above hard surfaces in most places. The remainder of the midpack is made up of dense facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm recent snow, lies over firm surface crust on south aspects up to at least 2600 m with softer snow found on north aspects. Minimal recent wind effect at higher elevations except in exposed ridge crests Profile at 2400m on Mt. Ogden found facets down 65cm with no results on column test. Cornices are huge!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm recent snow remains preserved on Northerly aspects and low angle terrain, on steep solar aspects a surface crust has formed. Some recent wind effect at higher elevations that seems limited to ridge crests. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. Cornices are huge.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High solar input have created crusts and moist snow on solar aspects at TL and below. Expect this condition to increase in elevation with rising freezing levels. SW winds have redistributed the snow pack at TL and ALP. The mid pack is supportive in deep areas but weak in shallow areas where it fails on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Another dusting overnight Thursday brings the total to 25cm in the last few days and 50cm since Saturday. A breakable suncrust can be found down 15cm in open areas and a second crust down 25cm on all aspects to treeline, higher on solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">10-20cm recent snow remains preserved on Northerly aspects and low angle terrain, on steep solar aspects a surface crust has formed. Some recent wind effect at higher elevations that seems limited to ridge crests. Profile at 2400m on Mt. Ogden found facets down 65cm with no results on column test. Cornices are huge!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm recent snow remains preserved on Northerly aspects and low angle terrain, on steep solar aspects a surface crust has formed. Some recent wind effect at higher elevations that seems limited to ridge crests. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. Cornices are huge!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">High solar input in the last few days created crusts and moist snow on solar aspects at TL and below. Wind scoured ALP features lost most of its snow to the lees of the mountains.  The mid pack is supportive in deep areas but weak in shallow spots where it fails on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Up to 50cm of new snow in the past week is still cold and dry on north aspects, and has been through several melt freeze cycles on south aspects. A breakable suncrust can be found down 15cm in open areas and a second crust down 25cm on all aspects to treeline, higher on solar aspects. The mid and lower snowpack is generally settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm recent snow remains preserved on Northerly aspects and low angle terrain, on steep solar aspects a surface crust has formed. Some recent wind effect at higher elevations that seems limited to ridge crests. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. Cornices are huge!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of recent snow remains preserved on Northerly aspects with a skiable temperature crust below 1700m. On solar aspects substantial surface crusts have formed. Extensive wind effect in the alpine with isolated sheltered areas. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. Cornices are huge!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunny skies and warm temperatures have created crusts and moist snow on solar aspects at tree line and below. There is widespread wind scouring to rock in exposed alpine features. The middle of the snowpack is supportive in deep areas but weak in shallow spots where it fails on buried facet layers in test results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">The surface snow has been moistened (and is now refrozen) on all aspects below 2000m and has been through several melt freeze cycles on solar aspects. Settled dry snow can still be found on high north aspects. The mid and lower snowpack is generally settled and strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of recent snow remains preserved on Northerly aspects with a skiable temperature crust below 1700m. On solar aspects substantial surface crusts have formed. Extensive wind effect in the alpine with isolated sheltered areas. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. Cornices are huge!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Dry low density snow remains preserved on Northerly aspects with a skiable temperature crust below 1700m. On solar aspects substantial surface crusts have formed. Extensive wind effect in the alpine with isolated sheltered areas. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunny skies and warm temperatures have created crusts and moist snow on all aspects at tree line and below and into the alpine on solar aspects. There is widespread wind scouring to rock in exposed alpine features. The middle of the snowpack is supportive in deep areas but weak in shallow spots.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Overnight, 5cm of new snow buried a crust on all aspects below 2000m and into the alpine on solar aspects. On high north aspects, the new snow covers settled dry snow. The mid and lower portions of the snowpack are generally strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Dry low density snow remains preserved on Northerly aspects with a skiable temperature crust below 1700m. On solar aspects substantial surface crusts have formed. Extensive wind effect in the alpine with isolated sheltered areas. Recent profiles show the Feb. 19 and Jan. 27 facets in the upper meter with hard to no results. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Amidst extensive wind effect and sun crusts in the alpine, pockets of dry low density snow can be found on Northerly aspects.  Expect a breakable to skiable temperature crust below 1700m. Ski crampons/crampons may be helpful to have on hand.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sunny skies and warm temperatures have created crusts and moist snow on all aspects at tree line and below and into the alpine on solar aspects. There is widespread wind scouring to rock in exposed alpine features. The middle of the snowpack is supportive in deep areas but weak in shallow spots.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A surface crust exists on solar aspects and an otherwise isothermal snowpack at lower below treeline elevations. Settled dry snow is preserved on north aspects in the alpine. The mid and lower portions of the snowpack are generally strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Amidst extensive wind effect and sun crusts in the alpine, pockets of dry low density snow can be found on Northerly aspects. Expect a breakable to skiable temperature crust below 1700m. Ski crampons/crampons may be helpful to have on hand. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A variety of snow surfaces exist from ice crust to wind crust to soft powder on high, northern aspects. Expect crust on all aspects below 1700 m. Surface hoar up to 1 cm is forming on the snow surface and will become a failure layer for future snow falls. Otherwise the deep snowpack is relatively strong and well settled.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warm temps and high solar input has created typical spring like conditions with moist snow on solar aspects from daytime heating, TL and below. Continuing SW winds have redistributed the snow pack, forming hard slabs in the ALP. The mid pack is supportive in deep areas, but shallow snowpack areas are weak and will break down fast with temp swings.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Spring melt freeze conditions exist at lower elev, and into the sub-alpine on S-SW asp. Dry snow may still be found on Northerly asp in the Alp, and isolated wind slabs at ridgetop. Isothermal snowpack can be observed at lower elevations on solar asp in the afternoon. At TL and above, on polar asp the mid, and lower snowpack is relatively strong.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A crust exists on the surface to ridgetop on solar aspects and at low elevations breaking down during the day. This tops 30-50cm dense snow above of the Feb 14 facet layer which is above hard surfaces in most places. The remainder of the midpack is made up of dense facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A variety of snow surfaces exist from ice crust to wind crust to soft powder on high, northern aspects. Expect crust on all aspects below 1700 m. Surface hoar up to 1 cm is forming on the snow surface and will become a failure layer for future snow falls. Otherwise the deep snowpack is relatively strong and well settled.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects (East to West) into the Alpine and a temperature crust on all aspects below 1800m. Soft snow still available on high North aspects. Surface hoar up to 10mm has formed in isolated, shaded areas and will become a failure layer for future snow falls. Otherwise the snowpack is relatively strong and well settled.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Warm temps and high solar input has created typical spring like conditions with moist snow on solar aspects from daytime heating, TL and below. Continuing SW winds have redistributed the snow pack, forming hard slabs in the ALP. The mid pack is supportive in deep areas, but shallow snowpack areas are weak and will break down fast with temp swings.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Spring melt-freeze conditions exist at lower elevations, and into the alpine on solar asp. The snowpack has even turned isothermal in the afternoon at lower elevations, on solar aspects. On Polar aspects at and above TL the surface snow remains dry, with a strong mid, and lower-snowpack. The March crusts and spotty unreactive SH is buried ~30cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Sun crust on steep solar aspects (East to West) into the Alpine and a temperature crust on all aspects below 1800m. Soft snow still available on high North aspects. Surface hoar up to 10mm has formed in isolated, shaded areas and will become a failure layer for future snow falls. Otherwise the snowpack is relatively strong and well settled.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow fell Friday with rain and no freeze below 1500m. The new snow now buries sun crust on steep solar aspects (East to West) into the Alpine, a temperature crust on all aspects below 1800m and  Surface hoar up to 10mm located in isolated, shaded areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 5cm of new snow becoming moist on solar aspects and creating thin slabs in ALP lees. Warm temps and high solar input have created sun crust on solar aspects TL and below. Snowpack becoming isothermal 1700m and below on all aspects. Generally strong mid-pack with exception in shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Warm temps and rain overnight have kept the snowpack isothermal at lower elevations. Above the rain line, 5cm of new snow is covering a melt-freeze crust into the alpine on solar asp, and surface hoar on dry settled snow on polar aspects. Strong alpine winds have likely blown the new snow into pockets of windslab in the alpine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A thick crust exists on the surface to ridgetop except on high north faces. This tops 30-50cm moist snow above of the Feb 14 facet layer which is above hard surfaces in most places. The remainder of the midpack is made up of dense moist facets and decomposing crusts, with early season ice crusts forming the base.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow fell Friday with rain and no freeze below 1500m. The new snow now buries sun crust on steep solar aspects (East to West) into the Alpine, a temperature crust on all aspects below 1800m and Surface hoar up to 10mm located in isolated, shaded areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow fell Friday with rain below 1800m. The new snow now buries sun crust on steep solar aspects (East to West) into the Alpine, a temperature crust on all aspects below 1800m and Surface hoar up to 10mm located in isolated, shaded areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10cm of new snow creating thin slabs in ALP lees. Warm temps and high solar input have created sun crust on solar aspects TL and below. Snowpack becoming isothermal 1700m and below on all aspects. Generally strong mid-pack with exception in shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">15-25 cm of new snow is covering a melt-freeze crust on solar aspects, surface hoar on dry settled snow on polar aspects, and a moist upper snowpack at lower elevations. Moderate-strong alpine winds will increase slab characteristics in the new snow. Cornices are large and fragile, and may be triggered by the increased load from new snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5-10 cm of new snow fell Friday with rain below 1800m. The new snow now buries sun crust on steep solar aspects (East to West) into the Alpine, a temperature crust on all aspects below 1800m and Surface hoar up to 10mm located in isolated, shaded areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-25 cm of snow has fallen at treeline and alpine elevations in the past three days accompanied by moderate to strong SW/W winds. The new snow sits over various sun crusts on steep solar aspects at all elevations, and over a temperature crust on all aspects below 1800 m. Minimal new snow at valley bottom with thin areas becoming isothermal.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 20cm new from convective flurries over past couple days redistributed by SW winds TL/ALP, overlies a variety of sun crusts and moist snow on solar aspects up to ALP. The overall snowpack is variable at TL and above with a supportive strong 1F to P midpack in the deeper areas to a weak facetted midpack in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">25-35 cm of new snow is covering a melt-freeze crust on solar aspects, surface hoar on dry settled snow on polar aspects, and a moist upper snowpack at lower elevations. Cornices are large and fragile, be sure to maintain good travel habits and give them a wide berth. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-25 cm of snow has fallen at treeline and alpine elevations in the past three days accompanied by moderate to strong SW-W winds. The new snow sits over various sun crusts on steep solar aspects at all elevations, and over a temperature crust on all aspects below 1800 m. Minimal new snow at valley bottom with thin areas becoming isothermal.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-35 cm of snow has fallen at treeline since March 19th with variable SW-NW winds. This storm snow sits over a sun crust on solar aspects, over a mix of surfaces on North aspects including facets and spotty surface hoar, and over a temperature crust at lower elevations. Minimal new snow at valley bottom with thin areas becoming isothermal.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 25cm new snow from convective flurries over past few days, redistributed by SW winds TL/ALP, overlies a variety of sun crusts on solar aspects up to ALP. The overall snowpack is variable at TL and above with a supportive strong 1F to P midpack in the deeper areas to a weak facetted midpack in shallow areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">30-45 cm of new snow is covering a melt-freeze crust on solar aspects, surface hoar on dry settled snow on polar aspects, and a moist upper snowpack at lower elevations. Cornices are large and fragile, be sure to maintain good travel habits and give them a wide berth. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">5-20cm of settled storm snow sits  on a thick crust that exists to ridgetop except on high north faces. This tops a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, none of which have been reactive in snowpack tests or recent avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-35 cm of snow has fallen at treeline since March 19th with variable SW-NW winds. This storm snow sits over a sun crust on solar aspects, over a mix of surfaces on North aspects including facets and spotty surface hoar, and over a temperature crust at lower elevations. Minimal new snow at valley bottom with thin areas becoming isothermal.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen at treeline since March 19th with variable SW-NW winds. This storm snow sits over a sun crust (up to ridge tops) on solar aspects, and over a mix of surfaces on North aspects including facets and spotty surface hoar, and over a temperature crust at lower elevations. Thin areas becoming isothermal below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Convective flurries and favorable SW winds have redistributed low density, new snow over hard windslab and varied crusts at TL/ALP elevations. This combination often creates a very poor bond at the interface and users should be wary of isolated slab development in open and/or steep features. Difficult travel BTL, w/ covered hazards and open water. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">30-45cm of recent storm snow is covering a melt-freeze crust on solar aspects and isolated pockets of surface hoar on polar aspects. Recent high freezing levels have created a moist upper snowpack at lower elevation which is now topped with a breakable crust. Cornices are large and fragile. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen at treeline since March 19th with variable SW-NW winds. This storm snow sits over a sun crust (up to ridge tops) on solar aspects, and over a mix of surfaces on North aspects including facets and spotty surface hoar, and over a temperature crust at lower elevations. Thin areas becoming isothermal below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen at treeline since March 19th with variable SW-NW winds. This storm snow sits over a sun crust (up to ridge tops) on solar aspects, and over a mix of surfaces on North aspects including facets and spotty surface hoar, and over a temperature crust at lower elevations. Thin areas becoming isothermal below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Convective flurries and favorable SW winds have redistributed low density, new snow over hard wind slab and varied crusts at TL/ALP elevations. This combination often creates a very poor bond at the interface and users should be wary of isolated slab development in open and/or steep features. Difficult travel BTL when the crusts break down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Strong southerly winds accompanied 10cm of new snow overnight.  The new snow adds to an existing load that sits atop the March 18th weak layer which presents as a crust on solar aspects and surface hoar on shaded aspects. March 18th is sensitive to skier triggering in areas where wind slabs have developed.  Cornices are large and fragile. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen at treeline since March 19th with variable SW-NW winds. This storm snow sits over a sun crust (up to ridge tops) on solar aspects, and over a mix of surfaces on North aspects including facets and spotty surface hoar, and over a temperature crust at lower elevations. Thin areas becoming isothermal below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen within the last week with variable SW-NW winds. This new snow sits over a sun crust (up to ridge tops) on solar aspects, over a temperature crust at lower elevations and over a mix of surfaces on North aspects including facets and spotty surface hoar. Thin snowpack areas are becoming isothermal below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of new snow with convective flurries and favorable SW winds have redistributed the low density, new snow over previous surfaces such as hard windslab and varied crusts at TL/ALP elevations. The snow pack varies throughout the region from strong supportive snow in deeper areas to weak facetted snow in the shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">40cm of snow has fallen this week over the March 18th sun crust and surface hoar. Below this is a strong mid pack of rounds at treeline and above. The below treeline snowpack has has experienced several melt freeze cycles.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Not much change to the snowpack in the past week. 5-20cm of settled storm snow sits over a thick crust that exists to ridgetop except on high north faces. This tops a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, none of which have been reactive in snowpack tests or recent avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen within the last week with variable SW-NW winds. This new snow sits over a sun crust (up to ridge tops) on solar aspects, over a temperature crust at lower elevations and over a mix of surfaces on North aspects including facets and spotty surface hoar. Thin snowpack areas are becoming isothermal below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen within the last week with variable SW-NW winds. This new snow sits over a sun crust (up to ridge tops) on solar aspects, over a temperature crust at lower elevations and over a mix of surfaces on North aspects including facets and spotty surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of new snow with convective flurries and moderate W-SW winds have redistributed the low density, new snow over previous surfaces such as hard windslab and changeable crusts at TL/ALP elevations. The snow pack varies throughout the region from strong supportive snow in deeper areas to weak facetted snow in the shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">40cm of snow has fallen this week over the March 18th sun crust and surface hoar. Short sunny spells are quickly affecting the top 15cm. Crusts have been seen to 2150m on due S aspects, likely higher in steep terrain. The mid pack of rounds is strong and supportive. The below treeline snowpack has has experienced several melt freeze cycles.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40 cm of snow has fallen within the last week with variable SW-NW winds. This new snow sits over a sun crust (up to ridge tops) on solar aspects, over a temperature crust at lower elevations and over a mix of surfaces on North aspects including facets and spotty surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40cm of snow has fallen within the last week. This snow sits over a sun crust on solar aspects, facets on North aspects and a temperature crust at lower elevations. Incoming snow ,wind and warm temps will add load to the current snowpack and widespread wind effect at upper elevations. Rain saturated snow is expected at lower elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of new snow with convective flurries and moderate W-SW winds have redistributed the low density, new snow over previous surfaces such as hard windslab and variable crusts at TL/ALP elevations. The snow pack varies throughout the region from strong supportive snow in deeper areas to weak facetted snow in the shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Ongoing snowfall and wind (up to 15cm in the past 24hr) has created reactive slabs. Snowfall totals of up to 55cm over the March 18th interface (this has been reactive just West of the park, on sheltered North aspects where it is surface hoar). The mid pack is strong and supportive. The below treeline snowpack has seen several melt freeze cycles.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">10-20cm of new snow is expected on Sunday with strong- extreme SW wind. This will create fresh wind slabs over a variety of old surfaces including a thick crust that exists to ridgetop (except on high N aspects) or old wind slab on N-E alpine slopes. Mid snowpack is well consolidated with the lower half composed of dense facets &amp; decomposing crusts</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-40cm of snow has fallen within the last week. This snow sits over a sun crust on solar aspects, facets on North aspects and a temperature crust at lower elevations. Incoming snow ,wind and warm temps will add load to the current snowpack and widespread wind effect at upper elevations. Rain saturated snow is expected at lower elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">5 to 25 cm of snow at treeline on Sunday with the most in the 93N. New wind slabs in alpine and exposed treeline areas with strong to extreme S-SW winds. Moist snow below 1500 m. 20-50+ cm now sits over the March 19 interface of crust on solar aspects and facets on north aspects. Nov basal facets still prominent in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10cm of HN with continued snowfall brings the recent HST up to 40cm. This new snow overlies previous surfaces such as hard windslab and variable crusts at TL/ALP elevations. The snow pack varies throughout the region from strong supportive snow in deeper areas to weak facetted snow in the shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Ongoing snowfall and wind (up to 35cm in the past 48hr) has created reactive slabs, and added significant growth to cornices. Snowfall totals of up to 75cm over the March 18th interface (this has been reactive just West of the park, on sheltered North aspects where it is surface hoar). The mid and lower snowpack is settled and strong. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">10-20cm of new snow is expected on Sun PM with strong- extreme SW wind. This will create fresh wind slabs over a variety of old surfaces including a thick crust that exists to ridgetop (except on high N aspects) or old wind slab on N-E alpine slopes. Mid snowpack is well consolidated with the lower half composed of dense facets &amp; decomposing crusts</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 25 cm of snow at treeline on Sunday in some areas. New wind slabs in alpine and exposed treeline areas from strong to extreme S-SW winds. 20-50+ cm now sits over the March 19 interface of crust on solar aspects and facets on north aspects. Moist snow below 1500 m. Snowpack becoming isothermal below 1300 m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of settled storm snow at treeline with the higher amounts up 93N. New wind slabs in alpine and exposed treeline areas with strong to extreme S-SW winds. 20-50+ cm now sits over the March 19 interface of crust on solar aspects and facets on north aspects. Nov basal facets still prominent in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Varied snowfall through the region. Up to 20cm settled HN in the Icefields Area. This new snow overlies previous surfaces such as hard windslab and variable crusts at TL/ALP elevations. The snow pack varies throughout the region from strong supportive snow in deeper areas to weak facetted snow in the shallow areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Another 30cm at Treeline brings our storm totals to ~50cm &lt;48 hours, and ~75cm in the last 72 hours! Strong Southerly winds and warm temperatures accompanying the new snow has formed storm reactive storm slabs. The March 18th layer is now buried 40-100cm depending on aspect and elevation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">10-20cm of new snow is bonding well to previous surfaces but expect the recent snow to become more reactive as it transitions to wind slab on tuesday. These wind slabs sit over a variety of old surfaces including a thick crust that exists to ridgetop (except on high N aspects) or old wind slab on N-E alpine slopes. Mid snowpack is well consolidated </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of settled storm snow at treeline with the higher amounts up 93N. New wind slabs in alpine and exposed treeline areas with strong to extreme S-SW winds. 20-50+ cm now sits over the March 19 interface of crust on solar aspects and facets on north aspects. Nov basal facets still prominent in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of snow fell on Sunday night, with the most around Sunshine and Bow Summit. Wind slabs exist in alpine and exposed treeline areas from strong winds during the storm. The March 19 interface of crust on solar aspects and facets on north aspects is below this, now down 20-50 cm. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread variability at the surface with up 20cm settled HN in the Icefields Area. New snow overlies previous surfaces such as hard windslab and variable crusts at TL/ALP elevations. The snow pack shows strength and good bonding in field tests but feels weak overall in the shallow regions like Whistlers/Portal creek and Maligne zones. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Since Friday, Rogers Pass has received ~85cm of snow at treeline! Strong Southerly winds and warm temperatures that accompanied the new snow has formed reactive storm slabs. The March 18th layer is now buried 40-100cm depending on aspect and elevation. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of snow fell on Sunday night, with the most around Sunshine and Bow Summit. Wind slabs exist in alpine and exposed treeline areas from strong winds during the storm. The March 19 interface of crust on solar aspects and facets on north aspects is below this, now down 20-50 cm. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of recent storm snow, with the most around Sunshine and Bow Summit, will be available for transport by the forecasted strong winds on Thursday to build wind slab. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The most recent storm snow is being redistributed by moderate winds, forming wind slabs in the ALP and TL. Warm daytime temps and overnight freezing will result in moist surface snow and crusts BTL. The HS is highly variable throughout the region with a strong supportive midpack in deeper areas and a weak unsupportive midpack in shallow areas. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Since Friday, Rogers Pass has received ~95cm of snow at treeline. The storm came in with warm temperatures and moderate to strong wind, forming storm slabs. These storm slabs remain reactive to skier triggering on specific terrain features in the Alpine and at Treeline. The March 18th layer is now buried 60-100cm depending on aspect and elevation. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of recent storm snow, with the most around Sunshine and Bow Summit, will be available for transport by the forecasted strong winds on Thursday to build wind slab. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of recent storm snow early this week, with the most around Sunshine and Bow Summit. Strong winds have formed wind slab at tree line and above. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread variability on the surface. Steady moderate SW flow, forming wind slabs on W through N aspects at TL and ALP. Inconsistent travel conditions and open water below 1800m. The snowpack shows strength and good bonding in field tests but &quot;feels&quot; weak in typically shallow snowpack regions like Whistlers/Portal creek and Maligne zones.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A fresh breakable crust on solar aspects may break down if the sun comes out this afternoon. Recent winds have built pockets of slab in alpine and treeline lees.  The March 18th layer (a crust on Solar aspets and isolated surface hoar on sheltered Northerly aspects) is now buried 60-100cm depending on aspect and elevation. Cornices are huge.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist surface snow on solar aspects will create a crust that deteriorates through the day. Previous SW wind formed wind slabs up to 30cm deep in the alpine &amp; exposed slopes at tree line. These wind slabs sit over a variety of old surfaces including a thick crust that exists to ridgetop except on high N aspects. Mid snowpack is well consolidated.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15-35cm of recent storm snow early this week, with the most around Sunshine and Bow Summit. Strong winds have formed wind slab at tree line and above. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Crusts exist up to ~1600m on all aspects and higher on solar aspects. Strong Southerly winds have formed wind slab at tree line and above. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread variability on the surface with 10cm of new snow and variable winds forming wind slabs on a variety of aspects at TL and ALP. Deteriorating travel conditions below 1900m. The snowpack shows strength and good bonding in field tests but &quot;feels&quot; weak in shallow snowpack regions like Whistlers/Portal creek and Maligne zones.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A fresh breakable crust on solar aspects may break down if the sun comes out this afternoon. Recent winds have built pockets of slab in alpine and treeline lees. The March 18th layer (a crust on Solar aspets and isolated surface hoar on sheltered Northerly aspects) is now buried 60-100cm depending on aspect and elevation. Cornices are huge.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Crusts exist up to ~1600m on all aspects and higher on solar aspects. Strong Southerly winds have formed wind slab at tree line and above. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10 cm of new snow in some areas with previous wind effect at treeline and above. Crusts exist up to ~2000 m on all aspects and higher on solar aspects. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread variability on the surface with 10-15cm of new snow and variable winds forming wind slabs on a variety of aspects at TL and ALP. Deteriorating travel conditions below 1900m. The snowpack shows strength and good bonding in field tests but &quot;feels&quot; weak in shallow snowpack regions like Whistlers/Portal creek and Maligne zones.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Up to a meter of snow last week has settled significantly over the March 18 suncrust and surface hoar. At treeline and above windward and lee features have a 15cm variable hard wind packed layer on the surface. Meltfreeze conditions below treeline, solar meltfreeze to mountaintop. Cornices are huge.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist surface snow on sun exposed slopes with a thick crust on all aspects up to 2000m. SW wind has formed wind slabs up to 30cm deep on lee slopes in the alpine. These wind slabs sit over a variety of old surfaces including a crust that exists to ridgetop except on high N aspects. Mid snowpack is well consolidated.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10 cm of new snow in some areas with previous wind effect at treeline and above. Crusts exist up to ~2000 m on all aspects and higher on solar aspects. The March 19 interface is down 20-50cm and consists of crust on solar aspects and facets on north aspects. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of new snow at treeline over previous crusts and wind effect. New wind slabs forming in alpine lee areas from moderate to strong SW-W winds. Moist snow on all aspects up to 1800 m and higher on solar aspects on Sunday. The March 19 crust interface is down 30-60 cm. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">HST of 10-30cm of new snow becoming moist TL and below on solar aspects. Shifting winds forming isolated wind slabs at TL and ALP. The snowpack shows good bonding in field tests in deeper snowpack areas, shallow snowpack regions such as Whistler/Portal and Bald Hills have bigger a potential for weak layers to wake up and are more complex to assess. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">15cm of new snow fell at treeline overnight, dwindling to rain below 1200m. Wind blasted surfaces exist below the new snow, suncrusts and meltfreeze conditions below treeline. Recent snow over the March 18th suncrust and surface hoar has settled significantly to about 70cm at treeline. Cornices are huge.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of new snow at treeline over previous crusts and wind effect. New wind slabs forming in alpine lee areas from moderate to strong SW-W winds. Moist snow on all aspects up to 1800 m and higher on solar aspects on Sunday. The March 19 crust interface is down 30-60 cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of new snow at treeline over previous crusts and wind effect. New wind slabs forming in alpine lee areas from moderate to strong SW-W winds. Moist snow on all aspects up to 1800 m and higher on solar aspects on Sunday. The March 19 crust interface is down 30-60 cm. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">HST of 10-30cm has settled to about 10cm of snow. Shifting winds forming isolated wind slabs at TL and ALP. The snowpack shows good bonding in field tests in deeper snowpack areas, shallow snowpack regions such as Whistler/Portal and Bald Hills have bigger a potential for weak layers to wake up and are more complex to assess. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A convective 15-30cm of new snow fell at treeline overnight Saturday and into the day yesterday, dwindling to rain below 1200m. Wind blasted surfaces and suncrusts exist below the new snow. BTL, expect spring melt-freeze conditions. Recent snow over the March 18th suncrust and surface hoar has settled to about 80cm at treeline. Cornices are large!</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20 cm of new snow at treeline over previous crusts and wind effect. New wind slabs forming in alpine lee areas from moderate to strong SW-W winds. Moist snow on all aspects up to 1800 m and higher on solar aspects on Sunday. The March 19 crust interface is down 30-60 cm. Basal facets exist in shallow areas east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is mix of crusts to 1800 m, and dry powder snow on north facing slopes above 1800 m. New snow, strong winds and cooling temps start Wed and with this we expect fresh, sensitive windslabs in the alpine. Treeline and below treeline elevations should become frozen and stay mostly frozen. Quite a variable spring snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">HST of 10-30cm has settled to about 10cm of snow. Increasing winds forming isolated wind slabs in open TL and ALP. The snowpack shows good bonding in field tests in deeper snowpack areas, shallow snowpack regions such as Whistler/Portal and Bald Hills have bigger a potential for weak layers to wake up and are more complex to assess. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">15-30cm of snow fell at treeline overnight Saturday and into Sunday; this was rain below 1200m. Wind blasted surfaces and suncrusts exist below the new snow, while the March 18th suncrust and surface hoar is buried ~80cm at treeline. Spring melt/freeze conditions prevail below treeline and on solar aspects to treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is mix of crusts to 1800 m, and dry powder snow on north facing slopes above 1800 m. New snow, strong winds and cooling temps start Wed and with this we expect fresh, sensitive windslabs in the alpine. Treeline and below treeline elevations should become frozen and stay mostly frozen. Quite a variable spring snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is mix of crusts to 1800 m, and dry powder snow on north facing slopes above 1800 m. New snow, strong winds and cooling temps have promoted some wind slab development.  Treeline and below treeline elevations should become frozen and stay mostly frozen. Quite a variable spring snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">New snow and steady SW winds building wind slab in open ALP and TL features. Snowpack shows strength and bonding in field tests; recurring instabilities are found close to surface. We are most concerned about potential to trigger deeper, persistent slabs (Fc, DH), especially as the snowpack changes with typical spring inputs (rain, sun, wet snow)</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Variable snow surfaces are present at the moment: 10-15cm settled powder on sheltered N aspects, thin wind-pressed surface skin below glacial toes, suncrust on solar aspects, and Spring melt/freeze crust below treeline. The March 18 suncrust/surface hoar is down ~80cm at treeline. Cornices, as always at this time of year, are large and fragile.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">10-15cm of new snow is expected thursday. This will create storm slabs which sit over old wind slabs on all but north facing slopes in the alpine. Mid snowpack is well consolidated with multiple decomposing crusts found near the base of the snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The snow surface is mix of crusts to 1800 m, and dry powder snow on north facing slopes above 1800 m. New snow, strong winds and cooling temps have promoted some wind slab development. Treeline and below treeline elevations should become frozen and stay mostly frozen. Quite a variable spring snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow in the past 24hrs now buries a crust up to 1800m, higher on steep solar aspects. New wind slab growth in the alpine down into tree line. Several persistent layers exist in the mid to lower snowpack and have been responsible for several large avalanches. These layers will remain a concern for some time due to their uncertainty.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 15cm of new snow sits on a thick crust that exists to ridgetop except on high north faces. This tops a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, none of which have been reactive in snowpack tests or recent avalanches. Large cornices observed overhead where good skiing can be found. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Up to 10cm of new snow is being blown into fresh windslabs and covering a variety of old surfaces: settled powder on sheltered alpine N aspects, windslabs/ wind pressed surfaces in exposed areas, a suncrust on solar aspects, and spring melt/freeze crust below treeline. Cornices, as always at this time of year, are large and fragile.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 15cm of new snow sits on a thick crust that exists to ridgetop except on high north faces. This tops a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, none of which have been reactive in snowpack tests or recent avalanches. Large cornices observed overhead where good skiing can be found. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">10-20cm of snow in the past 24hrs now buries a crust up to 1800m, higher on steep solar aspects. New wind slab growth in the alpine down into tree line. Several persistent layers exist in the mid to lower snowpack and have been responsible for several large avalanches. These layers will remain a concern for some time due to their uncertainty.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of new snow now buries a crust up to 1800m, higher on steep solar aspects. New wind slab growth in the alpine down into tree line. Several persistent layers exist in the mid to lower snowpack and have been responsible for several large avalanches. These layers will remain a concern for some time due to their uncertainty.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm of new snow arrived Wednesday night at Parkers ridge with much less further North and South. Winds are increasing to moderate speeds forming alpine ridgetop windslabs. The midpack is firm snow over weak basal facets and depth hoar near the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 10cm of new snow is being blown into fresh wind slabs and covering a variety of old surfaces: settled powder on sheltered alpine N aspects, wind slabs/ wind pressed surfaces in exposed areas, a sun crust on solar aspects, and spring melt/freeze crust below treeline. Cornices are large and fragile. The March 18 crust is buried ~80-100cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 15cm of new snow (TL and above on northerly terrain) sits on a supportive crust that exists to ridgetop except on high north faces. Overall a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, none of which have been reactive in snowpack tests or shown weakness in avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 30cm of new snow now buries a crust up to 1800m, higher on steep solar aspects. New wind slab growth in the alpine down into tree line. Several persistent layers exist in the mid to lower snowpack and have been responsible for several large avalanches. These layers will remain a concern for some time due to their uncertainty.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 40cm of recent snow buries a crust up to 1800m on all aspects (higher on steep solar aspects). New wind slab growth in the alpine down into tree line. Several persistent layers exist in the mid to lower snowpack and have been responsible for several large avalanches. These layers will remain a concern for some time due to their uncertainty.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">25cm of new snow arrived Wednesday night at Parkers ridge with much less further North and South. Winds are increasing to moderate speeds forming alpine ridgetop windslabs. The midpack is firm snow over weak basal facets and depth hoar near the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15cm of new snow fell overnight with strong S winds. Storm/ wind slabs cover a variety of old surfaces: settled powder on sheltered alpine N aspects, wind slabs/ wind pressed surfaces in exposed areas, a sun crust on solar aspects, and spring melt/freeze crust below treeline. Cornices are large and fragile. The March 18 crust is buried ~80-100cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Up to 40cm of recent snow buries a crust up to 1800m on all aspects (higher on steep solar aspects). New wind slab growth in the alpine down into tree line. Several persistent layers exist in the mid to lower snowpack and have been responsible for several large avalanches. These layers will remain a concern for some time due to their uncertainty.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of storm snow at treeline with more at higher elevations. Buried crusts up to 1800m on all aspects and to ridge crest on solar aspects. Small wind slabs in alpine lee areas. Several persistent layers exist in the mid to lower snowpack that can be a concern in thin areas, with significant warming or with larger triggers like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">20-30 cm of new snow arrived since Wednesday night at Parkers ridge with much less further North and South. The midpack is firm snow over weak basal facets and depth hoar near the ground.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of new snow in 48hrs with strong S winds fell on top of the April 7th sun crusts, wind pressed surfaces and melt freeze crusts at low elevations. The March 18 crust is down 90cm. A very strong dense mid and lower pack sits on up to 50cm of decomposed crusts and large facetted crystals near the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 20cm of new snow  at TL and above on northerly terrain. This sits on a supportive crust that exists to ridgetop except on high north faces (starting to break down mid day). Overall a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, which haven't produced test results or recent avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of storm snow at treeline with more at higher elevations. Buried crusts up to 1800m on all aspects and to ridge crest on solar aspects. Small wind slabs in alpine lee areas. Several persistent layers exist in the mid to lower snowpack that can be a concern in thin areas, with significant warming or with larger triggers like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of storm snow at treeline with more at higher elevations. Buried crusts up to 1800m on all aspects and to ridge crest on solar aspects. Small wind slabs in alpine lee areas. Several persistent layers exist in the mid to lower snowpack that might be a concern in thin areas, with significant warming or with larger triggers like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Light winds shifting to the north, new sun crust on solar asp to TL and temperature crust all aspects BTL below 1900m. Previous new snow now settled. March 19th crust is buried 10-50cm+ on solar aspects to 2200m. Mid-pack is firm and bridging a weak lower snowpack in deep areas. Weak snowpack particularly where shallow (exposed alpine features).</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">30cm of new snow on Friday/ Saturday with strong S winds fell on top of the April 7th sun crusts, wind pressed surfaces and melt freeze crusts at low elevations. The March 18 crust is down 90cm. A very strong and dense mid and lower pack sits on up to 50cm of decomposed crusts and large facetted crystals near the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 40cm of recent low density snow at treeline and above with minimal wind effect. This sits on a supportive crust that exists to ridgetop except on high north faces. Overall a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, which haven't produced test results or recent avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of storm snow at treeline with more at higher elevations. Buried crusts up to 1800m on all aspects and to ridge crest on solar aspects. Small wind slabs in alpine lee areas. Several persistent layers exist in the mid to lower snowpack that might be a concern in thin areas, with significant warming or with larger triggers like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of storm snow at treeline with more at higher elevations. Buried crusts up to 1800m on all aspects and to ridge crest on solar aspects. Small wind slabs in alpine lee areas. Several persistent layers exist in the mid to lower snowpack that might be a concern in thin areas with significant warming or with larger triggers like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Varied surface conditions though the region. In the Icefields, the mid-pack is firm and bridging a weaker, lower snowpack. Shallow regions like Maligne, and all BTL locations are susceptible to wide, diurnal temperature swings (up to ~30 degree temp. difference), making for extremely weak, wet, hazardous conditions, especially on any solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A surface crust exists on all but northerly aspects, into the alpine. At treeline and above, a settled 30cm of snow sit on the April 7th sun crust and wind pressed surfaces. The March 18 crust is down 90cm. A very strong and dense mid and lower pack sits on up to 50cm of decomposed crusts and large facetted crystals near the ground</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of storm snow at treeline with more at higher elevations. Buried crusts up to 1800m on all aspects and to ridge crest on solar aspects. Small wind slabs in alpine lee areas. Several persistent layers exist in the mid to lower snowpack that might be a concern in thin areas with significant warming or with larger triggers like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of settled recent snow at treeline. Crusts up to around 2000m on all aspects and to ridge crest on solar aspects. Several persistent layers exist in the mid to lower snowpack that might be a concern in thin areas with significant warming or with larger triggers like cornices which are prevalent in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Transitioning into spring conditions. Southerly aspects expect a crust that will break down by late morning; northerly aspects TL and above may hold dry snow depending on freezing level. Persistent intense solar and warm temps will continue to destabilize snowpack structure increasing the likelihood of natural and human triggered avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Spring melt-freeze conditions exist at lower elevations, and higher on solar aspects. Polar aspects are still holding dry snow in the alpine and at treeline. The April 7th layer is down ~20-40cm depending on aspect and elevation, and the March 18th crust is down ~60-1m. The mid and lower snowpack is very strong and dense.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 30cm of recent snow at treeline and above with minimal wind effect. This sits on a supportive crust that exists to ridgetop except on high north faces. Overall a well consolidated snowpack with the lower half composed of dense facets and decomposing crusts, which haven't produced test results or recent avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">15 to 30 cm of settled recent snow at treeline. Crusts up to around 2000m on all aspects and to ridge crest on solar aspects. Several persistent layers exist in the mid to lower snowpack that might be a concern in thin areas with significant warming or with larger triggers like cornices which are prevalent in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard surface crusts in the morning, then wet snow in the afternoon. High elevation north aspects will still hold dry snow. Another solid overnight freeze is expected for Friday morning, then deteriorating rapidly as the day warms up. There are several persistent layers n the mid to lower snowpack will wake up over the next 48 hr.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Spring has Sprung! Expect a crust on solar aspects that will break down early in the day; polar aspects at TL and above may hold dry snow depending on freezing level. Persistent intense solar and warm temps will continue to destabilize snowpack structure increasing the likelihood of natural and human triggered avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Spring melt-freeze conditions exist at lower elevations, and higher on solar aspects. Polar aspects are still holding dry snow in the alpine and at treeline. The April 7th layer is down ~20-40cm depending on aspect and elevation, and the March 18th crust is down ~60-1m. The mid and lower snowpack is very strong and dense.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p><p class="p_CC664AAA"><span class="s_AA239A9B"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Up to 30cm of recent snow in the alpine with minimal wind effect. This sits on a supportive crust that exists to ridgetop except on high north faces. Overall a well consolidated snowpack. With warming temps we expect the snowpack to become isothermal over the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Hard surface crusts in the morning, then wet snow in the afternoon. High elevation north aspects will still hold dry snow. Another solid overnight freeze is expected for Friday morning, then deteriorating rapidly as the day warms up. There are several persistent layers n the mid to lower snowpack will wake up over the next 48 hr.</span></p>
{"blocks":[{"key":"6jde7","text":"Alpine areas have been heavily affected by the past week of strong winds and wind slabs are widespread at tree line and above. Ridges and ribs are stripped free of snow while lee and cross-loaded terrain have deep deposits of wind loaded snow. The November crust is down 30-100cm and is producing anywhere from moderate to no results.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"6jde7","text":"Warm temps today and over the next few day may create a sun crust in open solar slopes. Observed snowballing and pin wheeling from the solar slopes today.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"ahme3","text":" Alpine areas have been heavily affected by the past week of strong winds and wind slabs are widespread at tree line and above. Ridges and ribs are stripped free of snow while lee and cross-loaded terrain have deep deposits of wind loaded snow. The November crust is down 30-100cm and is producing anywhere from moderate to no results.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"ajqua","text":"Alpine areas have been heavily affected by the past week of strong winds and wind slabs are widespread at tree line and above. Ridges and ribs are stripped free of snow while lee and cross-loaded terrain have deep deposits of wind loaded snow. The November crust is down 30-100cm and is producing anywhere from moderate to no results.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"ajqua","text":"Alpine areas have been heavily affected by the past week of strong winds and wind slabs are widespread at tree line and above. Ridges and ribs are stripped free of snow while lee and cross-loaded terrain have deep deposits of wind loaded snow. The November crust is down 30-100cm and is producing anywhere from moderate to no results.  Moist snow has been seen on steep solar aspects...So watch for another crust to get buried into the future.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"ajqua","text":"Alpine areas have been heavily affected by the past week of strong winds and wind slabs are widespread at tree line and above. Ridges and ribs are stripped free of snow while lee and cross-loaded terrain have deep deposits of wind loaded snow. The November crust is down 30-100cm and is producing anywhere from moderate to no results.  Moist snow has been seen on steep solar aspects...so expect a surface crust on these slopes.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"ajqua","text":"If the amount of snow is more than forecast or comes earlier with the winds, be mindful of fresh wind slabs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"4mh2a","text":"Alpine areas have been heavily affected by the past week of strong winds and hard wind slabs are widespread at tree line and above. Ridges and ribs have been previously stripped free of snow while lee and cross-loaded terrain have deep deposits of previous wind loaded snow.  The November crust is down 30-100cm and is still producing anywhere from moderate to no results.  Faceting has started near the Nov. crust and is something that will be followed closely as more load gets deposited.  Alpine temperatures reached near +2c on Monday.  Expect some surface crusts from this warming event or from last week's warming, especially on solar aspects.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9u8b9","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"a4u7h","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e11ig","text":"Warm temps started the day on Tuesday and once again a crust related to rain was developed overnight up to 2300m.  As the new snow moves in over the next 24hrs we expect a variety of different snow surfaces to get buried including windslabs, surface hoar, crusts related to last weeks warm temps and facets.  Windslabs will be harder to see and we have to see how this new snow bonds to the underlying crust.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"dbnha","text":"Up to 30cm of snow fell in the past 24hrs with only isolated variable winds in upper elevation.  This new snow is overlying a variety of surfaces from surface hoar (up to 2100m) and crusts (solar aspects) that formed in the big warm up last week as well as hard windslabs.  Carefully evaluate the bond of this new snow as it begins to strengthen over the next few days.  The November crust is down 50-80cm now and continues to produce variable results.  The snowpack felt a bit cakey along ridgelines on Wednesday so be watching for winds to increase making these windslabs more reactive.  In some areas below 2000m the snowpack was moist...","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"36af","text":"The new snow is over a variety of surfaces, surface hoar in isolated locations up to 2100m as well as crusts from last week warm temps and the early storms rain, as well the hard wind slabs.  The Nov. 6 crust is down 50-80cm there is a wide range of result on this layer it may become more sensitive with the new load uses caution in unsupported terrain.  Isolated wind slabs all aspects in the alpine.  New SH growth at all elevations.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"6h3m3","text":"Surface hoar is still building up to 2000m. Above that there is no significant growth. But the alpine surface hoar is still intact in most places. Surface faceting is also quite obvious, the snow is cold and \"grabby\" on the skis right now. The Dec 9 surface hoar continues to be elusive. Holes today didn't have it, and the new snow isn't cracking or settling. Speaking of new snow, there has been a lot of settlement in the snowpack. Storm snow is about 25cm at treeline. Also of note, the Nov crust is very thick and supportive in Commonwealth drainage. Faceting above/below the crust didn't appear to be a problem today.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"24igb","text":"Surface hoar continues to grow in sheltered areas at lower elevations. Due to the cold temperatures there is also significant surface faceting occurring. There remains very little wind effect on the recent snow, even in the Alpine, however forecasters did note some snow movement at mountain top today. The recent 25 to 30cm of low density surface snow sits over a wide variety of layers, including hard wind slabs, crusts and surface hoar. During the storm, the region experienced a widespread avalanche cycle involving this new snow, but in recent days there has been little to no activity. The November rain crust is faceting out, but the condition of the crust is becoming quite variable. In some areas it remains dense and easily carries the weight of a skier, while in other areas it has broken down significantly.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"21mi7","text":"A hint of wind last night moved some snow around up high which created a few non-reactive windslabs. We seem to have a slightly different snowpack in each drainage. In the Hero's Knob area the new snow rests on a solid mid-pack made up of either a windslab, or a thick re-frozen layer from the warm spell awhile back. In many  places the crust is smooth and its easy to scrub off the storm snow. For now all the crusts are well settled and hard to trigger.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7a902","text":"Winds are expected to increase to 80km/h on Tuesday.  Expect wind slabs in the alpine, especially just behind ridge crests and lee features.  One concern with this slabbing is that it will sit on top on a 1cm crust that was formed 10 days ago during the warm spell and could release on this crust.  Approach the alpine with caution and take the time to dig and look at this bond. The November 5 crust is about 60cm down and is showing faceting around it. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"23esl","text":"Up to 10cm of recent snow at treeline combined with the recent low density snow is being moved around by winds creating new windslabs in open areas up to 20cm thick.  These new windslabs are overlying a variety of snow surfaces from sun crusts, surface hoar and previous windslabs.  Evaluate this interface as you travel and feel for that drummy hollow feeling.  Deeper down the November crust still persists and should still be in your mind.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e4b75","text":"Thursday is expected to bring 10-15cm of snow for a total of about 30-40cm of loose snow that is starting to move around in the alpine.  The concern now is when this turns into a fresh wind slab, it will be sitting on top of the December 8 crust which will be about 30-40cm down.  This 0.5cm crust was formed during the warm spell 10 days ago and is quite a smooth surface for a slab to release on.  Approach tree line and lee features with your radar on.  With all this snow and wind coming, cornices will begin to grow.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"46s65","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2p3sg","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e4b75","text":"Our storm didn't pan out last night, but the winds sure did! Lots of transport today with new slabs at treeline and alpine elevations. As the slabs grow, the Dec 8th layer may become reactive. It all depends on the specific loading pattern. Expect the Dec 8th to be down anywhere from 20-50cm. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"489r5","text":"We managed to get a few more centimeters added to the snowpack yesterday and today. This actually helped the travel and ski quality down low today. Any open area at treeline and above has seen significant wind transport. There was a noticeable windslab that formed during the day today. This will essentially sit on the Dec 9th crust/facet layer left over from the warm spell. So far this layer is not reacting, but being a crust, we can expect faceting above it. In which case it could quickly become more reactive. The Dec 9th is down about 20-40 depending on loading patterns. The Nov5th crust is down about 80cm at treeline and again, it seems to be cooperating with the rest of the snow pack.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"3mjfn","text":"A few centimeters came in last night, which helped the skiing. Oddly enough, the winds haven't taken a huge toll on the treeline elevation. Great skiing was had today in sheltered treeline areas. The alpine is a different story...and not in a good way. Extensive wind transport has crossloaded most features and stripped the westerly aspects to gravel. Windslabs are widespread, and plump. Overall the snowpack is doing well with no scary layers. The Dec 9th and Nov 5th are down 45cm & 90cm at treeline.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"esmud","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"du4oo","text":"EDIT 1030am Sunday: We've received 20-35 cm of snow over Saturday night. Extreme westerly winds have also contributed to a higher than expected hazard rating. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e10j","text":"Up to 25cm of new snow,  with very strong winds lee slopes would have much more snow possibly up to 1m.  20-100cm overlying the Dec 8th facet crust interface.  Wide spreed wind affect in Alpine in to open tree line features.  Caution for reverse loading with the strong North winds.  Found soft to hard slabs. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e10j","text":"Up to 5cm of new snow over night,  30-80cm overlying the Dec 8th surface hoar, facet, crust interface.  Widespread wind affect in Alpine in to tree line features.  Caution for reverse loading with the strong North winds.  Settlement in the upper snow pack might make it more sensitive to skier traffic around tree line features.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8ha6n","text":"40 to 50cm of snow fell in a very short period of time, which has overloaded the snowpack. Winds were strong out of the north during the storm, so expect widespread wind slabs at Treeline and above. The Dec 8th layer of surface hoar/crust/facets remains on the radar, especially with this new load. The Nov rain crust is now deeply buried in the snowpack, and while it hasn't been reactive recently, it could easily wake up with the new snow load. Field observations were very limited today, and forecasters will be going out with eyes wide open on their next field day - the snowpack has experienced significant change!","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"dt9no","text":"The storm snow has settled quickly and now sits at about 30cm in sheltered areas. Northern winds have taken a toll in open terrain and formed soft windslabs in many areas. The alpine has extensive wind affect at the moment. Alpine and treeline windslabs are now \"layered\" with slabs of varying vintages. We have seen evidence of avalanches within these layered wind slabs. The Deb 8th and Nov 5th layers are still out there and have reacted in many areas under the new load. We suspect its mostly the Dec 8 crust/facet layer that most guilty, but its also appeared that the Nov 5th has also been a culprit. See the  Avalanche Summary for more details.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"45flj","text":"Strong winds is the main thing to talk about with regards to the snowpack.  Winds over the past 24hrs have been strong out of the SW and most alpine areas have been highly affected.  In some areas we are seeing windslabs overloading the basal November crust triggering large avalanches that are running to the valley floor.  Expect to encounter windslabs at open areas at treeline and expect the windslabs to fail in steep or crossloaded areas down 40-60cm at the Dec 8th interface.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e027a","text":"5cm of snow over the past 24hrs is overlying the recent wind slabs that were developed during the Christmas break.  Alpine areas are significantly wind affected with some ridgelines scrubbed down to rock and other filled with plump slabs.  In some areas the the overburden of the new wind loaded snow awoke the facets overlying the Nov crust triggerring isolated deep slab avalanches up to sz 3.   At treeline windslabs are more specific in nature and unsupported or crossloaded features should be places to avoid.  Hollow or drummy sounds are a good indication you are moving into wind affected terrain. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e1esk","text":"2 to 3cm of new snow overnight, adds to the 5cm that fell yesterday. Alpine areas are significantly affected by wind, with widespread wind slabs present. These are now somewhat disguised by the recent snow. The depth and character of these slabs is highly variable. Dig down and evaluate the recent interface before entering a line. The November crust layer has been active in a few recent avalanches which indicates it's potential if overloaded. This layer is also highly variable in character, and will be on our minds for some time to come.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"18fel","text":"Up to 15cm of recent snow overlies a variety of previous surfaces. This surface snow is soft and fluffy in some areas, and wind affected in others, especially as you transition to the Alpine. Extensive wind slabs were formed in the pre-Christmas storm, and it is worth noting that the storm arrived with extreme Northerly winds, which switched to extreme SW winds in the following days. Therefore, the region has buried wind slabs on virtually all aspects. The depth and character of these slabs is highly variable, and it is worth a dig before committing to more aggressive terrain. Forecasters are still tracking the Dec 8th layer (surface hoar, facets, crust) now down 40 to 80cm, but this layer has been inactive in recent days. The November rain crust is also worth keeping an eye on, as it has been responsible for a few recent large avalanches.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"18fel","text":"This surface snow is soft and fluffy in some areas, and wind affected in others, especially as you transition to the Alpine. Extensive wind slabs were formed in the pre-Christmas storm, and it is worth noting that the storm arrived with extreme Northerly winds, which switched to extreme SW winds in the following days. Therefore, the region has buried wind slabs on virtually all aspects. The depth and character of these slabs is highly variable, and it is worth a dig before committing to more aggressive terrain. Forecasters are still tracking the Dec 8th layer (surface hoar, facets, crust) now down 40 to 80cm, but this layer has been inactive in recent days. The November rain crust is also worth keeping an eye on especially in shallow snowpack areas where it might be possible to skier trigger this layer,  If or when it slides it will end up bing a large avalanche.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"531kk","text":"Generally a strong snowpack.  The alpine consists of a couple of generations of wind slabs.  The first being the surface wind slabs(top 10cm) that have formed in the last couple of days. The second wind slab is below the surface one which goes down about 30-40cm which was formed during the strong variable Christmas winds. Approach alpine features with wind slabs on your mind. The Dec. 7 and Dec 15 layers are about 40 to 80cm down and are still identifiable but mostly unreactive.  The November 5 crust is mostly a concern for triggering in steep shallow areas where the facets overtop of the Nov. crust are much more prominent","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"phqf","text":"For December its s good snowpack!  The main concern is the generations of windslabs that currently exist in the upper snowpack.  As you transition from the trees into the more wind affected treeline and alpine be looking for these windslabs and be thinking about thick to thin snowpack areas.  Thin weak areas will be the most likely places to trigger these windslabs that may also step down to the basal november crust. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"e7ksl","text":"Winds on Friday were increasing and as s result we were seeing more pronounced windslabs development in the region especially in the alpine and into treeline.  Our Snowpack mainly consist of generations of windslabs overlying a relatively strong mid pack with the Basal November rain crust at the lower elevations.   For december it has been a fairly stable snowpack with the windslabs in the upper snowpack as the primary concern but that is all likely to change with the incoming storm.  As we did pre Christmas, we are expecting to see avalanches in the upper snowpack and the possibility of the basal facets and November crust becoming overloaded and failing triggering large avalanches. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"6d7f2","text":"Pronounced windslab development in the region especially in the alpine and into treeline.  Our Snowpack mainly consist of generations of windslabs overlying a relatively strong mid pack with the Basal November rain crust at the lower elevations.   For december it has been a fairly stable snowpack with the windslabs in the upper snowpack as the primary concern but that is all likely to change with the incoming storm.  As we did pre Christmas, we are expecting to see avalanches in the upper snowpack and the possibility of the basal facets and November crust becoming overloaded and failing triggering large avalanches.   Forecasters were getting cracking in open areas around burstall pass. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"67qhj","text":"10 to 15cm of snow fell in the past 24 hours adding to the 5 to 10cm from Saturday. Unfortunately, the winds have been strong out of the SW during much of the snowfall which has led to widespread new wind slab development in Alpine and Treeline areas. It has been a very windy couple of weeks, so the upper snowpack mainly consists of several \"generations\" of wind slab. Conditions vary extensively across the region, so take the time to dig down and evaluate the snowpack. The mid pack is relatively strong and well settled for December. Forecasters continue to monitor the Nov crust layer buried deeply in the snowpack. This layer has been occasionally active, producing large avalanches, but has remained quiet in recent days. Shallow snowpack areas, or transitioning from thick to thin snow depths are the most likely areas to trigger the deeper instability.","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":266,"length":4,"style":"ITALIC"},{"offset":266,"length":4,"style":"BOLD"}],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"6pj73","text":"This last weekend brought us up to 25cm of snow along with strong winds. The result is widespread wind slabs in the Alpine and isolated areas of tree line.  There are now several generations of wind slabs in the upper snowpack.  As you transition from tree line to the alpine, take the time to dig and evaluate what is going on with the snowpack.  We have a generally strong mid pack that sits overtop of the November 5 crust.  Our greatest concern with the Nov. crust is in shallow areas where the facets around the crust are more pronounced.  Cornices are growing fast so it is a good time to give them lots of space.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"h80u","text":"Lots of variability within the upper snowpack currently with some areas highly wind affected and others with 25cm of low density snow on the surface.  Being heads up for these windslabs up to 40cm deep is the key thing to note.  As you transition into wind affected terrain look and feel for the surface of the snow to become wind affected.   We did see some light to moderate SW winds on Tuesday moving snow around but it felt like the first day not in a hurricane.  In some areas the overhead cornices look large and looming so be sure to keep your head looking up. Otherwise the midpack in the region continues to settle and strengthen with the basal november crust near the ground still in our minds despite no recent avalanches on this interface.  Thin areas are places to tread carefully as you may awaken the basal layers.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"fqu8","text":"Lots of variability within the upper snowpack currently with some areas highly wind affected and others with 25cm of low density snow on the surface.  Being heads up for these windslabs up to 40cm deep is the key thing to note.  As you transition into wind affected terrain look and feel for the surface of the snow to become wind affected.   We did see some light to moderate SW winds on Tuesday moving snow around but it felt like the first day not in a hurricane.  In some areas the overhead cornices look large and looming so be sure to keep your head looking up. Otherwise the midpack in the region continues to settle and strengthen with the basal november crust near the ground still in our minds despite no recent avalanches on this interface.  Thin areas are places to tread carefully as you may awaken the basal layers. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7mr8s","text":"Our snow pack condition varies greatly within the range. The northern portion looks wind hammered...more like clobbered actually. Hard windslabs, and even sastrugi are obvious in any open alpine area. As you move south it improves and looks better. Our trip today was around Mt Murray where the alpine windslabs were isolated and fairly well settled. The midpack generally feels solid, except for rocky thin areas-no surprise there. Below treeline is supportive with good travel. We did notice a very thin suncrust from today on steep treeline solar and new surface hoar up to about 2300m. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"agdl8","text":"The overnight temps were in the -20's last night (Thursday night) and kickstarted the surface faceting and surface hoar growth. The top 20cm is low density and offers good skiing in treeline areas. In valley bottoms the surface hoar is growing, up to 10mm in places. Our trip today was near Purple Knob. We only travelled up to treeline, but noticed a variable depth snowpack. In many places it was only 60-80cm with a poor base. In the deeper areas the midpack was solid feeling with some noticeable buried windslabs. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"c3m11","text":"Surface hoar growth and surface facetting is widespread below 2000m due to the cold temperatures and clear nights.  Otherwise the upper snowpack is generally low density with a well settled midpack.  Concerns regarding the basal facets and crusts will be with us for the season so we will almost always be telling people to avoid travelling in thinner shallow snowpack areas especially in steeper terrain.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"1qot0","text":"Strong winds on Monday has moved snow around to create wind slabs in the Alpine and parts of tree line.  Expect new soft slabs to begin developing with the incoming storm and strong winds.  These new slabs will not have had time to bond to the strong mid pack.  Approach open terrain with caution.  The most recent surface hoar can be found at tree line and below and will be buried by the incoming snow.  Approach steep open terrain at treeline and below treeline with caution.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"9mn9a","text":"3cm of new snow fell in the past 24hrs. The extreme SW winds continue, and have created widespread wind slabs at all elevations on south, north and east aspects. Only the most sheltered areas below treeline have escaped this. Today forecasters dug a pit at treeline and discovered multiple wind slab layers that all produced sudden planar failures at the different interfaces. In addition, ski cutting produced surface sluffing in steep sheltered terrain below treeline today indicating that the new snow is not bonding well to the old surface. If the forecasted snow arrives, these observations indicate that a natural avalanche cycle will occur at all elevations.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"fm4rn","text":"15-20cm of snow fell over the past 24hrs under the influence of strong SW winds and warm temperatures.   Widespread windslabs are being observed in alpine terrain and also in open areas at treeline that are failing down 30-40cm at the recent storm snow interface.  The midpack is generally well settled and the November crust today was unreactive in rutschlock test at 2200m.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"fm4rn","text":"Widespread windslabs were observed in alpine terrain and also in open areas at treeline that are failing down 30-40cm at the recent storm snow interface.   The slab varies from Hard slab to soft slabs. The midpack is generally well settled over November crust that is not producing much in results in the test pits.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"fm4rn","text":"Widespread windslabs were observed in alpine terrain and also in open areas at tree line, the storm interface down 20-40cm has been tightening up and not near as reactive to compression test and ski cutting.   The slab varies from Hard slab to soft slabs, would still use caution when approaching slopes with wind affect. The midpack is generally well settled over November crust that is not producing much in results in the test pits.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"4ltau","text":"Wind slabs as far as the eye can see. Seriously, that's  the big story right now. It seems all elevations and aspects have a layer of new, hard AND breakable windslab right now. The good news is that the mid pack is well settled with only a few layers of concern. The concerning layers are variable in their location, and tend to be the layers of windslabs reacting, not the deeper layers. We found \"drummy\" snow today in the Murray Moraines area today and suspect that the entire range has that snow quality right now. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"20d77","text":"I wish I had better news, but the widespread wind effected snow is still the main feature of our snowpack. A profile near Purple Knob had a well settled mid pack with the Nov 5th down 165cm and a surprising lack of depth hoar or facets near it. It seems the warm snowpack temperatures have kept the bottom layers from \"rotting\" out and becoming weak. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"anrd9","text":"A skiff of snow covers the widespread wind slabs in the Alpine and into tree line.  A test profile at Burstall Pass today revealed the sheers in the upper 50cm are tightening. Despite the wind slabs, the actual skiing was fair and you could stay on top of the surface without breaking through. The cornices right now are pretty large for this time of year.  With the strong winds coming on Tuesday, be on the lookout for new wind slabs forming.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"fuqvs","text":"Widespread wind slabs in the alpine and into tree line.  The very strong winds over the last 2 days might just lay down another slab if there is any snow left to transport.  The cornices are large for this time of year.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"40fpe","text":"Anyone who has read a Snowpack Summary in the last week can probably sense where this is going...","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9460n","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"66tkp","text":"Widespread wind effect is the major theme for the next while. Until we get more snow, the windslabs will be a problem. The good news is that the cold temps are helping to break them down and the snow stability is fairly good given the widespread nature of the slabs. If the cold does last, remember to check in on the deeper layers as they will start to break down and become weaker.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"40fpe","text":"Widespread wind effect is the major theme for the next while. Until we get more snow, the windslabs will be a problem. The good news is that the cold temps are helping to break them down and the snow stability is fairly good given the widespread nature of the slabs. If the cold does last, remember to check in on the deeper layers as they will start to break down and become weaker.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"40fpe","text":"Widespread wind effect is the major theme for the next while. Until we get more snow, the windslabs will be a problem. The good news is that the cold temps are helping to break them down. If the cold does last, remember to check in on the deeper layers as they will start to break down and become weaker.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"2uql7","text":"The windslabs are still there and widespread.  Not much change until we get some more snow.  Approach cross loaded features and lee loaded zones along ridges with extra care.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"eua7l","text":"Well some facetting is making for light snow in the trees but anywhere that could be wind affected is.  No snow in quite some time now is essentially making the skiing pretty grim out there.  Great travel though!  Just keep windslabs in your mind though also think about what will be when it snows again!","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"eua7l","text":"A few cms of snow fell over the past 24hrs but its going to take a bunch more to change the avalanche hazard.  Windspread wind affect is being found in all open areas.  Some softer facetted snow is being found in the trees but skiing is limited due to widespread tracks of late.  We just have to be patient and wait and see for when a significant weather pattern comes in to create a change. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"5e28f","text":"10cm of recent snow is adding to the dribbles of snow that we have received over the past few days.  Winds have generally been light.  This new snow is overlying a variety of snow surfaces from surface hoar and facets at lower elevations and windslabs and bare ground at the upper elevations.  How this new snow bonds to these surfaces will be critical to evaluate in the coming days.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cuabo","text":"Well, it seems our weather man was suffering from  dyscalculia yesterday. We were expecting 15cm, but got up to 51cm on Thursday night. This sits on a variety of old surfaces that will be slow to bond with the new snow. The most interesting (and nerve racking) thing about this new snow is how easily it wants to settle and bond with itself. Within an hour we saw it shift from loose dry avalanches to a more cohesive, almost slab character. It will take VERY little input for this to become a slab problem. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cuabo","text":"Thursday nights snow amounts very from valley to valley 15-40 cm. This sits on a variety of old surfaces that will be slow to bond with the new snow.  Avalanches are more likely in areas that have been affected from the wind or sun and the new snow becomes more cohesive, developing slab character. It will take VERY little input for this to become a slab problem. There is lots of low density snow available for transport and lee loading.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8atgh","text":"We spent the day in the Black Prince area today and found the near continuous flurries kept adding to the snowpack. Down low had about 20cm from the last few days, and higher had about 35cm. While that drainage is fairly sheltered, we did note that alpine winds were blowing snow around and creating new windslabs in the alpine.  It's safe to expect the regional alpine zone will have reactive windslabs on any lee (east) aspect. We may also have wind \"pressing\" slabs on the windward sides as well. This new snow sits on old surfaces which generally aren't a problem. The one exception to this is a narrow elevation band at treeline where the old slabs started to facet (weaken) during last week's cold snap. Steep convex rolls deserve some caution as the buried windslabs may be triggerable.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"el32t","text":"Another 30cm of new snow fell in the last 24 hours, bringing recent storm snow totals to between 60 and 70cm. So far this snow remains low density at lower elevations, but today at 2500m forecasters observed a change starting. The winds were moderate to strong from the SW and were quickly forming new surface wind slabs with some isolated cracking and whumpfing at ridge-crest. In addition, snowpack tests today indicate that all the recent storm snow is failing on the old wind slab surface down 60cm. Test results were variable ranging from very easy to moderate. Once the surface snow gains a bit more density, these new slabs will be quite sensitive to triggering.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"el32t","text":"Another 15cm of 24hour snow, bringing the storm snow to 50-60cm.   At treeline and below, the storm snow is bonding relatively well to the hard wind slab underneath.  On Tuesday, in open areas at treeline and above, the winds were intense and  have started to slab up the top 30cm+ and is reactive to skier traffic.  Expect to find  wind slabs up to 100cm thick, especially in lee features and cross loaded gullies. Open areas at treeline and above will need to be approached with caution.  Watch for cracking around your skis.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"aqp02","text":"Lots of new snow out there. We have anywhere from 35-60cm of settling storm snow from the last couple of days. Currently, this snow is low density in the valley bottoms, but stiffens up as elevation is gained. Alpine and treeline winds have begun to create fresh windslabs on eastern aspects. There are also buried windslabs within the storm snow. The Jan 29 (hard windslab/storm snow) interface is slower to bond than expected. Lots of avalanche activity on it in the past 24 hours. Deep layers are still hanging in there and so far not failing wit the new load.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"aqp02","text":"Lots of new snow out there. We have anywhere from 35-60cm of settling storm snow from the last couple of days. Currently, this snow is low density in the valley bottoms, but stiffens up as elevation is gained. Alpine and treeline winds have begun to create fresh windslabs on eastern aspects. There are also buried windslabs within the storm snow. The Jan 29 (hard windslab/storm snow) interface is slower to bond than expected.  Less avalanche activity seen today but no real alpine observations.  Winds slab are forming and suspect they will be touchy in the right spot.  Deep layers are still hanging in there and so far not failing wit the new load.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"4jnso","text":"Some steep solar aspects may have a sun crust.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"9l10o","text":"Read this line twice:","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"7jv98","text":"The snow just keeps coming!","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3da4d","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"c6hc9","text":"We rarely get to say that! ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8ulga","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1reah","text":"With all of this recent snow we are seeing multiple layers of windslabs form. So far this slab complex is bonding OK within itself, but steep, unsupported slopes could have failures within the multiple slabs. The Jan 29th/fresh windslab interface is still concerning. That January layer was exposed for a long time, which typically means it will be slow to bond. That layer could be down as much as a meter in places. Now being a Rockies forecaster, its quite hard to forget the deeper layers. It seems to be cooperating so far and it isn't a huge red flag at the moment, but its still in the back of our minds.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7eim7","text":"We are looking at about 60cm of settled snow from these recent storms and just over 2m total snow at treeline. Today we saw very little wind affect anywhere other than the north spray lakes area. More than one comment was made among us forecasters on how it was almost eerie to have this much snow and no major avalanche concerns. We do have some concerns with windslabs in wind prone areas and how they are bonding with the Jan 29th layer, but we don't have our usual deep persistent layer haunting us. First a global pandemic, and now a Kananaskis snowpack with no depth hoar!!! Who would have thought we'd see both of those in a single lifetime let alone a single winter?","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7eim7","text":"We are looking at about 60cm of settled snow from these recent storms and just over 2m total snow at tree line. The interface with the storm snow is progressively getting stronger but take the time to dig and evaluate this interface before committing to larger features. Some wind effect in the alpine and our usual concerns for lee features and cross loaded gullies. First a global pandemic, and now a Kananaskis snowpack with no depth hoar!!! Who would have thought we'd see both of those in a single lifetime, let alone a single winter?","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7eim7","text":"We are looking at about 60cm of settled snow from these recent storms and just over 2m total snow at tree line. The interface with the storm snow is progressively getting stronger but take the time to dig and evaluate this interface before committing to larger features. Some wind effect in the alpine and our usual concerns for lee features and cross loaded gullies.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7eim7","text":"We are looking at about 60cm of settled snow and just over 2m total snow at tree line. The interface with the storm snow is progressively getting stronger but take the time to dig and evaluate this interface before committing to larger features. Some wind effect in the alpine and our usual concerns for lee features and cross loaded gullies.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"dl6at","text":"Lots of surface faceting with these cold temperatures. There is about 60cm of settled snow overlying the Jan 29 wind slab interface. Take the time to dig and evaluate this interface as there is still variability with it.   Some wind effect in the alpine and our usual concerns for lee features and cross loaded gullies.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8gki6","text":"Surface Faceting making it easy to get pretty good sluffs going in steeper terrain, entraining some mass.  60cm of settled snow overlying the Jan 29 wind slab interface. Take the time to dig and evaluate this interface as there is still variability with it, as well check for crusts on the south facing slopes.  Wind effect in the alpine and our usual concerns for lee features and cross loaded gullies.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bmmuv","text":"EAST SIDE OF SPRAY LAKES ROAD: There is significantly less snow on this side.  The ski quality was good but not great coverage. the Nov. crust will be a problem, in the shallower snow pack. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"97ehb","text":"Lots of surface faceting out there. The top 20cm is cold and grabby, but loose with few slab properties. A profile today had sub-surface temps that are still relatively warm, which means limited mid pack faceting. The Jan 29 interface is down about 50cm with a hint of faceting above it. You'll know it when you find it, it is very, very solid. Our profile had a few weaknesses show up, but generally it was well bonded and solid. So far the cold has spared our good snowpack on the west side of the road.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"97ehb","text":"Wind slabs are apparent in the exposed alpine, but generally pretty good surface conditions for skiing. The surface faceting is also helping to keep the snow soft and skiable. The Jan 29th interface is still on the radar. Its down 50-60cm and is worth checking on if you're venturing out into uncharted terrain.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"ce6p9","text":"Surface wind slabs are evident in exposed areas in the alpine but still providing good skiing.  There is evidence of some slab avalanches starting near ridge lines within the top 30-40cm and running to mid path. Surface faceting is evident in the top of the snowpack.  The Jan 29th interface is down around 50cm and is still on our radar and is worth checking on if you are venturing into unchartered terrain.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"66c8k","text":"The sun is really starting to have some strength to it and should be on your radar if you are travelling close to sun exposed slopes.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cjl1t","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"c0rq4","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6dlk4","text":"The alpine has widespread wind slabs in the upper 40cm that are still providing good skiing as long as they are not too dense. Take the time to investigate these wind slabs so as to not be surprised in the density change. Cracking around your skis is a good indicator of this density change. The Jan 29 interface is down about 50-60cm and is producing a shear.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cjl1t","text":"The alpine has widespread wind slabs in the upper 40cm that are still providing good skiing as long as they are not too dense. Take the time to investigate these wind slabs so as to not be surprised in the density change. Cracking around your skis is a good indicator of this density change. The Jan 29 interface is down about 50-60cm and is producing a shear.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7khhb","text":"Fast and loose. The snowpack is facetted with weak surface snow, which is making for fast skiing as the snowpack warms up. We are also finding subtle windslabs on rolls at treeline, many of which are from the cold, sinking/downflow winds of the cold snap last week. While not reacting, they are sending the odd shiver down our back. It feels as though they want to move but they just aren't. The midpack is still solid and sitting on a decent base. Winds did pick up today at treeline and alpine elevations, we may see fresh windslabs on easterly aspects.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"bkuo6","text":"Watching how quickly the wind changed the snow's distribution over night it is quite clear that the cold snap turned our snowpack into sugar...and now the wind is blowing it all away! I'm sort of kidding. Many areas are blown to gravel, or old hard surfaces, but there are still lots of new windslabs out there. These will be sitting on top of facets, and touchy in steep, wind exposed areas. The good news is the deeper layers are still playing along and not failing. But remember, in times of rapid change (like now) its best to let those layers re-gain your trust. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"1ricj","text":"The effects of the recent winds are noticeable with windslabs in open terrain at treeline and above.  These windslabs are 10-20cm thick in areas travelled on Saturday but we can expect them to increase in depth and reactivity as winds continue overnight.  Any windslab that starts in the upper snowpack will likely step down to the Jan 29th persistent interface down 40-60cm.  Watch for these problems along ridgelines, and in lee terrain mainly on N and E aspects. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"arrba","text":"Extreme winds on Sunday are stripping all the remaining snow from windward aspects and depositing that snow into lee and cross-loaded features. Wind slabs are widespread at Treeline and above, and can even be found in open areas at lower elevations. The depths of the wind slabs are highly variable (5 to 80cm), as is the sensitivity to triggering. In exposed Alpine areas expect hard, dense wind slab conditions, but as you loose elevation these slabs are softer and potentially more triggerable. Be mindful of rapidly changing conditions as you travel through the terrain.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7toqs","text":"Field observations in the Spray Valley were limited today due to avalanche control operations on EEOR. Weather stations indicate that up to 25cm of new snow fell at Treeline elevations. Winds through the storm were extreme from the SW, so widespread wind slab conditions are expected. In the Alpine these slabs could be very dense, whereas at Treeline the slabs may be more soft in nature and potentially more human-triggerable. All lee and cross-loaded terrain should be approached with caution. Slab depths and sensitivity to triggering will be highly variable, so be mindful of rapidly changing conditions as you travel through the terrain.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"32h1q","text":"The recent snow has been affected by the strong winds on friday forming windslabs in open alpine terrain and isolated areas at treeline.  These slabs are 10-20cm thick where observed today but forecasters were being conservative in treeline features.  Moderate sheers were noted within the upper storm snow and no reactivity was observed on the Jan 29th interface down 70cm.  The big concern now is windslabs in the alpine in open areas.  If you feel drummy or hollow snow start seeking conservative terrain or supported low angles slopes.   ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"32h1q","text":"The recent snow has been affected by the strong winds on friday forming windslabs in open alpine terrain and isolated areas at treeline.  These slabs are 10-20cm thick where observed today but forecasters were being conservative in treeline features.  Moderate sheers were noted within the upper storm snow and no reactivity was observed on the Jan 29th interface down 70cm.  The big concern now is windslabs in the alpine in open areas.  If you feel drummy or hollow snow start seeking conservative terrain or supported low angles slopes.   ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"648aa","text":"We often have a distinct weather pattern each season, and this year it is abnormally strong winds. Last night and earlier today we had alpine gusts at over 150km/hr, and valley bottom winds in the 30-40km range. Needless to say, there's yet another layer of wind slabs in open areas and widespread wind effect near ridges. Lots of exposed rock and gravel out there right now too. Having said that, there are still sheltered areas that but up to the main ranges that will likely hold snow.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"5sn85","text":"The strong winds have created widespread windslabs in open areas in the alpine and a more variable windslab at treeline.  The cold facets layer that developed in the previous weeks is now buried down 40-50cm at treeline and the Jan 29th is down closer to 60-70cm.  The sheers on the facet layer are highly variable so dig down and check these interfaces before committing to a slope. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"98bnk","text":"Lots of buried windslabs out there right now. Overall we have really good coverage, but at times today we caught ourselves saying how loaded some alpine slopes look. These slopes all have multiple layers of windslabs that are so far sticking together and seemingly OK. We do have the voice in the back of our heads that warn of the Feb 14th facet layer and the Jan 29 hard slab layers. These are down 60cm and 100cm respectively, and worth having a look at.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"em9mr","text":"The forecasters dug a profile at treeline today and found about 10-20cm of loose snow overlying a 20cm wind slab and did produce a clean sheer.  There was evidence of several other generations of wind slabs as well. Generally a well consolidated snow pack but worth digging and looking at the top meter before committing to bigger lines.  The alpine sure looked loaded by wind and will get another dose of it on Monday.  These wind slabs and the loading in the alpine is the reason we are rating the hazard at \"Considerable\".","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8h6c9","text":"The most important things happening are in the upper 50cm of the snowpack. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"j5io","text":"The forecasters measured 0c at 2200m today and definitely noticed the warmth penetrating the snowpack below this elevation and settling it.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"e3g69","text":"Wind slabs should be on your radar.  There are several generations of wind slabs in the upper snowpack and the one closest to the surface has been skier triggered over the weekend. To add to that, snow and wind will add yet another fresh wind slab on the surface. Lee features and gullies look  especially primed for triggering especially with the fresh wind slab that should form Monday night.  This is a time to approach open areas at treeline and the alpine with respect and take the time to dig and evaluate the bonds between the wind slabs.  There has been skier triggered avalanches in K-Country and Banff National Park which is an indicator that conditions are not completely stable.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"v3tj","text":"It is also time to start thinking about the south facing slopes.  If the sun is out and it is hot out, the steeper southern slopes could be a concern for avalanching.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"c75fk","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6i0h6","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"esnrj","text":"This last storm dropped 15cm of snow along with strong winds.  The alpine and tree line have widespread wind slabs overlying a previous generation of wind slab.  There have been several avalanches on either this recent wind slab or the wind slab that is buried about 30-50cm down.  One cornice triggered avalanche also caused a surface slab to release.  With these warming temperatures and recent loading, cornice failures are on our radar.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"533nl","text":"Expect to see some moist snow on steeper solar aspects that will be a crust in the morning hours.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"3afqj","text":"Recent snow from earlier in the week is settling.  This snow is overlying a windslab down 10-20cm that was seeing some isolated cracking today in the Aster lake area.  Deeper in the snowpack there are two layers that we are following closely.  The Feb 19th Facets down 40-60cm and the Jan 29th interface down 60-100cm.  Windslabs (buried and near the surface) in the upper snowpack are likely to step down to one of these layers that are within the top meter.  These layers are subtle at treeline but very pronounced in the Alpine.  Dig down and assess these layers.  Forecasters today avoided big slopes in the alpine due to windslabs over these interfaces.  Moist snow was also found up to 2000m by midday.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"3afqj","text":"Given the warm day, expect a crust on southern aspects and possibly even western aspects. Recent snow from earlier in the week is settling.  This snow is overlying a windslab down 10-20cm that was seeing some isolated cracking today in the Aster lake area.  Deeper in the snowpack there are two layers that we are following closely.  The Feb 19th Facets down 40-60cm and the Jan 29th interface down 60-100cm.  Windslabs (buried and near the surface) in the upper snowpack are likely to step down to one of these layers that are within the top meter.  These layers are subtle at treeline but very pronounced in the Alpine.  Dig down and assess these layers.  Forecasters today avoided big slopes in the alpine due to windslabs over these interfaces.  Moist snow was also found up to 2000m by midday.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"j8sd","text":"Temperature crusts can be expected up well into the alpine on solar aspects and even on western aspects and on all aspects except pure north below treeline.  This will be a layer to pay attention to as it get buried here this spring. The upper snow pack consists of a variety of windslabs that are overlying two inportant layers.  The feb 19th facets as well as the Jan 29th interface.  Despite not seeing much activity on these layers over the past few days they are still forefront in our minds.  If anything the recent warm weather helped these layers to strengthen but the overlying windslabs are still stiff, and able to propagate if triggerred from a thin weak area.  Dig, be curious and evaluate these interfaces as you go.  Forecasters have felt drummy windslabs above treeline all week.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"6pptn","text":"We did get a few cm's of new snow today, which is welcome. In most areas the recent warmth has taken a toll with widespread crusts up to treeline elevations. Sunny aspects will now have a thinly buried crust up to alpine elevations. On the shady sides, there is still a series of stacked windslabs that are becoming less reactive as the snowpack cools.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"b3oni","text":"A walk to Tent Ridge today had 5-10cm low density snow on top of an insulated crust from the past few days. This crust is about 4cm thick and more pronounced on solar aspects. At treeline, the underlying crust was replaced with a hard windslab that was basically in the surface. A quick hole had the Feb 19th interface down 50-60cm and inconsistently reactive in tests. Despite a well settled snowpack in tests, we still bailed from the ridge early, suspecting reactive windslabs in the immediate lee.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"aomn1","text":"5 to 15cm of convective snow fell in the past 24hrs. The snowfall amounts vary considerably across the region. This new snow overlies a crust on solar aspects, and in many cases this new snow will have turned moist by Monday afternoon, producing a new surface crust by Tuesday morning. On non-solar aspects expect the recent snow to be sitting over a wide variety of previously formed wind slabs. These slabs vary considerably in depth and distribution. Recent snowpack tests indicate that the buried persistent weak layers of Feb 19 and Jan 27 are still present within the top 50 to 80cm, but generally the test results have been in the moderate to hard range.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"9gacd","text":"A very cold start to the day on Tuesday kept the new crusts frozen on solar aspects until the afternoon. Expect a few layers of sun crust on SE through W aspects. On non-polar aspects at Treeline and above there are several generations of wind slab in the upper 60 to 80cm of the snowpack. These slabs are highly variable, and it is worth taking the time to dig down and evaluate the snowpack before committing to bigger terrain. Forecasters are still monitoring the Feb 19 and Jan 27 layers.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"a0ab8","text":"It is sure feeling Springlike out there but there is still a few things happening in the snowpack. On solar aspects, expect to find a crust in the early morning hours and then turn to moist snow later on.  The sun has a lot of punch now so choose your route carefully in terms of overhead hazards like cornices and wet loose avalanches on southern aspects.  The hazard is likely to go up during the day with the sun and moist snow.  In other words, the day would start at Moderate and quickly change to Considerable with warming and solar radiation.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1k9sb","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"aqq5q","text":"The forecasters found that there is still variability in the top 60cm of the snowpack.  We mostly found several buried wind slabs down 15cm and 40cm overlying less dense layers.  Good skiing and dry snow will still be found on North and NE aspects.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"90uk0","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2teqt","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"a0ab8","text":"It is sure feeling Springlike out there but there is still a few things happening in the snowpack. On solar aspects, expect to find a crust in the early morning hours and then turn to moist snow later on.  The sun has a lot of punch now so choose your route carefully in terms of overhead hazards like cornices and wet loose avalanches on southern aspects.  The hazard is likely to go up during the day with the sun and moist snow.  In other words, the day would start at Moderate and quickly change to Considerable with warming and solar radiation.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1k9sb","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"aqq5q","text":"The forecasters found that there is still variability in the top 60cm of the snowpack.  We mostly found several buried wind slabs down 15cm and 40cm overlying less dense layers.  Good skiing and dry snow will still be found on North and NE aspects.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"90uk0","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2teqt","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"v93p","text":"The snowpack continues its transition to Spring. Moist snow on Saturday up to at least 2600m on solar aspects, and likely higher. This will turn into a crust by morning, but will quickly melt again by late morning on Sunday. Expect loose wet avalanches on solar aspects and sensitive cornices when they exposed to sun/heat. On non-solar aspects there are still some buried wind slabs in the upper 60 to 80cm of the snowpack that are worth investigating before committing to bigger terrain.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"dtj7b","text":"The snowpack continues its transition to Spring. Sunday was the warmest day of the Spring so far with barely freezing temperatures Saturday night.  This caused many wet loose avalanches on solar aspects on Sunday.  If Sunday night is clear, expect a crust on solar aspects on Monday and if it is cloudy, then the solar aspects might not have refrozen. In either case, solar radiation will play a factor in deteriorating the conditions, even on cloudy days. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"b16et","text":"On non-solar aspects there are still some buried wind slabs in the upper 60 to 80cm of the snowpack that are worth investigating before committing to bigger terrain.  Be alert on the changing snow conditions under your skis.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"atlvv","text":"With the heat from this last weekend, all solar aspects have melted during the day and frozen at night. With these kind of Spring conditions, timing and aspect is everything.  The alpine appears to be wind affected except for sheltered north aspects.  On non-solar aspects there are still some buried wind slabs in the upper 60 of the snowpack that are worth investigating before committing to bigger terrain.  Be alert on the changing snow conditions under your skis.  There are plenty of big cornices out there so take the time to plan your trip to avoid them.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"atlvv","text":"Melt freeze cycle seems to be the name of the game right now!  Melting during the day and becoming less stable and freezing at night.  With these kind of Spring conditions, timing and aspect is everything.  The alpine appears to be wind affected except for sheltered north aspects.  On non-solar aspects there are still some buried wind slabs in the upper 60 of the snowpack that are worth investigating before committing to bigger terrain.  Be alert on the changing snow conditions under your skis.  There are plenty of big cornices out there so take the time to plan your trip to avoid them.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"atlvv","text":"Melt freeze cycle seems to be the name of the game right now!  Melting during the day and becoming less stable and freezing at night.  On Wednesday the surface of the snow didnt begin to break down until mid afternoon and winds and temps kept it cool.    With these kind of Spring conditions, timing and aspect is everything.  The alpine appears to be wind affected except for sheltered north aspects.  On non-solar aspects there are still some buried wind slabs in the upper 60 of the snowpack that are worth investigating before committing to bigger terrain.  Be alert on the changing snow conditions under your skis.  There are plenty of big cornices out there so take the time to plan your trip to avoid them.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"7qthp","text":"Crusts are being observed up to the peaks on solar aspects but surprisingly, some dry snow is still being found on northern aspects down to 2000m.  You have to be creative with you lines but good skiing was still found on Thursday.  In general the ski quality is only good on the polar aspects and then on solar its all about timing.  Corn snow was found today at 11am but we didnt want to be out much later than that!  Early starts are important as it aspect and whats overhead...","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"chiou","text":"It sounds like we had some light snow that has buried the sun crusts and other various layers. With that we expect thin wind slabs in the alpine. The question will be how well they've bonded to the underlying layers. Given the warm temperatures, they will probably stick OK. Aside from the windslabs, we are dealing with a well settled spring like snowpack. Dry snow on polar aspects and refrozen, slightly buried crusts on sunny slopes.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"9b8tt","text":"10-15cm of new snow has fallen over the past 36hrs with wind affect only in alpine areas.  This new snow is very low density and sluffing easily in steeper terrain.  Especially in areas where it is overlying the previous melt freeze crust.  Two main things to be aware of are new windslabs in the upper snowpack in alpine areas and sluffing on anywhere this new snow is overlying the temperature crust.  As with spring, the weather can change quickly so be aware that if the sun does come out, stability will quickly deteriorate and natural avalanche activity will initiate.  Keep a keen eye trained on the local weather.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"56v5m","text":"Expect a mix of recent snow and new wind slabs in the alpine.  The forecast snow will most likely be low density with the cooler temperatures, so expect some sluffing in steeper terrain. The two main things to keep an eye out for is for new snow accumulation and the formation of new wind slabs.  With Spring time, the weather can change quickly and the snowfall can sometimes be far more than forecast and be very localized. The same goes if the sun comes out in between snow squalls; it can make the snow change quickly, especially on solar aspects. Use your mountain sense and evaluate each area carefully. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cn6qa","text":"There should be 5-10cm of new snow by Tuesday morning for up to 20cm of snow in the past 48hrs.  This amount can vary quite a bit and be very localized with the convective Spring storms, so use your mountain sense and evaluate each area carefully. The two main things to keep an eye out for are: ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"35ehl","text":"1)  Newly formed wind slabs, especially near ridge lines and lee features.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1d9i1","text":" 2)  Sluffing in steep terrain with the new snow as well as spindrift off higher cliffs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"fql3h","text":"If the sun is out, expect the new snow to change quickly on solar aspects.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"4mbh2","text":"15-20cm of recent snow is overlying the March 19th interface.  Winds were generally light to moderate in the Alpine out of the SE and isolated windslabs are building in alpine areas along ridgelines and cross-loaded features.  Carefully evaluate the bond with the new snow and the March 19th crust on the solar aspects where the bond is the most susceptible to fast sluffing.  AS winds increase on Thursday expect windslabs to become more reactive in alpine areas. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cks59","text":"Generally about 15cm of recent snow overlying the March 19 interface with isolated wind effect. Carefully evaluate the bond with the new snow and the March 19th crust on the solar aspects where the bond is the most susceptible to fast sluffing. This is Spring, so conditions and weather forecasts are all over the map.  Be prepared for fast changing conditions with snowfall amounts, wind and solar radiation. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"1tc20","text":"Only a few cm of snow has fallen over the past 24hrs with generally light winds.  The key things to be aware of are windslabs in the upper snowpack along ridgelines and in crossloaded features.  Some cracking has been observed in immediate lees but the slabs do not extend far downslope.  The March 19th interface is down 20-40cm and producing moderate sheers.  The quality of the sheer is different where it overlies a suncrust or a more wintery snowpack.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cu03s","text":"We had a pulse of snow last night that bumped the recent snow amounts to 20cm at treeline. As expected, it was convective in nature, which means amounts will vary from place to place. Its likely the overnight snow settled quickly today given the generally warm temperatures. On that note, we had moist snow up to 2000m today. The two biggest issues with all the recent snow are surface windslabs and the Mar 19 interface. The slabs are on all aspects, but limited to immediate lee areas. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"aacl5","text":"Isolated windslabs are being found in alpine areas but only limited reactivity along ridgelines and immediate lees.  Tomorrow will be a big change though as winds increase into the strong range with 20-40cm of new snow in alpine areas.  Expect windslabs to become more widespread at Alpine and treeline likely failing at the storm snow interface.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"5q041","text":"Only a few cm's had fallen by the time forecasters left the field Sunday at midday, but it was snowing hard. The bond at this new interface so far appears good, but wind slab formation was observed in open areas at Treeline. These slabs were already up to 20cm thick and some cracking was observed. Monday could see 15 to 25cm more snow with strong NW winds. If this comes true, expect to find widespread wind slabs through the terrain.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"5dpqn","text":"20 to 30cm of snow fell overnight depending on elevation. Some limited wind effect was observed at 2400m and above, but there were limited Alpine observations today. In most cases this recent snow appears well bonded at lower elevations, but observations on a solar aspect indicate that there could be a shear of concern down 30cm. This will be one to watch for the next couple of days, especially considering that several avalanches were observed in the Alpine today despite the limited visibility.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"4h394","text":"The recent storm snow of up to 30cm remains dry on northerly aspects, but was moist on the solar side by midday. By morning expect snow on SE through W aspects to have a surface crust. At treeline and below the recent snow is bonding well, but in the Alpine there is a different story. Wind slabs are evident on all aspects except west. The natural avalanche cycle is tapering off, but loaded slopes in the Alpine are primed for human-triggering.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"4h394","text":"The recent storm snow of up to 30cm remains dry on northerly aspects, but was moist on the solar side by midday. By morning expect snow on SE through W aspects to have a surface crust. At treeline and below the recent snow is bonding well, but in the Alpine there is a different story. Wind slabs are evident on all aspects except west. The natural avalanche cycle is tapering off, but loaded slopes in the Alpine are still in a human-triggering phase.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8kraa","text":"The dry snow is getting harder to find. Today wasn't especially warm, but all the weather stations were above zero by noon. The good news is the moderate warmth will help those pesky windslabs stick to the other layers. North aspects will preserve the alpine windslabs. The lower elevations are really feeling the freeze/thaw cycles. Snow is moist by early afternoon and is creeping higher and higher every day.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cmvu7","text":"Valley bottom snow was moist by 11am. Treeline hung in there and still had dry snow as of 1200. It likely stayed that way due to cloud cover. The most notable snowpack feature is the widespread wind effect. Any open area at treeline and up has a 5-10cm thick windslab. There are sheltered areas at treeline holding good snow, but they are small and isolated. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"f9ofp","text":"No new snow and little wind is keeping our snowpack on the slow to develop program. The mild freeze/thaw cycles are helping with settlement and bonding within the upper layers. Which is good, but it also means the crusts are slowly consuming our dry snow patches. Alpine windslabs remain on most aspects and are proving to be stable, but not fantastic skiing. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"cpk66","text":"Up to 12cm of new snow overlies widespread wind slabs in the Alpine, as well as some at Treeline. On solar aspects the surface snow has turned moist by midday. Later in the day on Tuesday the wind will pick up speed and begin to form new surface slabs in the Alpine.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"1qrlk","text":"Winds were light on Tuesday and as a result there wasnt much change in the current snowpack structure.  10-12cm of snow is overlying a variety of different snow surfaces in the alpine with isolated windslabs at cols and crossloaded features.  With winds increasing on Wednesday, these slabs may become more reactive and easier to find.  Surface snow was moist by midday on solar aspects.  At treeline and below travel is fast in the morning on surface crusts and mushy in the afternoon.  Early starts with careful consideration of overhead hazards already in the sun is critical.   ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"3p8s0","text":"Well the winds arrived over the past 24hrs and they left there mark on the snowpack.  A breakable windcrust was pretty widespread in the alpine and hooky skiing was the word of the day.  The only dry powder skiing we found was at treeline and below on pure north aspects.  Solar aspects have a melt freeze crust that is supportive in the morning, and less snow as the day warms up.  15-20cm of snow is expected overnight and it will be important to check the bond between this new snow and the underlying surface.  One good thing is the wind is forecast to be light so new windslabs may only be isolated to wind affected terrain such as cols and ridgelines.  pay close attention as you transition into wind affected terrain. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"9j6kq","text":"We received 20-25cm of new snow last night that stayed cold for most of today. Only valley bottoms had moist, heavy snow. In most places this new snow sits on a frozen crust that offers good support. We did find one steep roll at treeline that for some reason didn't have the frozen crust. Instead, it was insulated moist snow that whumphed on a couple of occasions. Once there is a slab on that moist snow, expect an avalanche. An overall lack of wind today kept the slab threat low. That will change once there's wind. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"c6r7c","text":"The close to 30cm snow that fell recently is beginning to be moved around by the winds creating windslabs in the upper elevations and even isoalted areas at treeline.  THese slabs are 20-40cm thick and failing at the recent storm snow interface.  On northern aspects this snow is overlying a winter snowpack while on E, S and W aspects this snow is overlying a melt freeze crust developed earlier in the week.   The bond on these two layers differs so be sure to check this interface.  At treeline, again forecasters got a few large settlements in treeline areas on southern aspects where the snowpack was wet and isothermal.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"c3rv3","text":"Another 20cm of snow fell overnight on Friday bringing our recent snowfall totals from the past few days up to 40-50cm.  This snow has been affected by strong variable winds that have created new reactive windslabs in alpine areas on all aspects that are failing on a storm snow interface down 40-60cm.  In some sheltered areas the windslabs is also buried under the recent snow making it more subtle and easy to underestimate.   Warm temps are promoting rapid settlement in the upper snowpack so this problem is likely to be active for the next few days.  Cooler temps forecast for Sunday will help stabilize these windslabs a bit, but a skier triggered event on the South side of Heros knob indicates there is potential for human triggerring.  Solar radiation is also strong at this time of year so start early and be mindful of decreasing stability on solar aspects later in the day.  ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8o4db","text":"It feels like we have a lot of snow out there right now, and none of it is in true spring condition. Its still a winter snowpack with a couple of tricky interfaces. There's about 40cm of recent snow on top of an older crust or windslab (depends on aspect). In most cases these layers are cooperating, but in the odd place they aren't meshing together very well. Its important to not let the surface layers fool you into thinking its a no-brainer of a snowpack. Ya gotta literally dig a little deeper and have a look at these deeper layers. Its a surprisingly variable snowpack right now with potential for surprises. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"14tnf","text":"Another 5 to 10cm of new snow fell in the last 24 hours. This brings recent storm totals to between 50 and 60cm. This storm snow sits on a crust on solar aspects, and may have thin crusts interspersed within the storm snow. The storm snow has remained mainly low density at upper elevations, but be on the lookout for both surface and buried wind slabs formed by both the \"traditional\" winds (SW) and by up-slope conditions (NE). Recent snowpack tests indicate moderate shears down between 50 and 70cm, so take the time to explore the local conditions as you travel. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"6ohev","text":"A few more cm's fell in the last 24hrs. The storm snow over the past week now totals between 40 and 60cm and is settling rapidly on solar aspects. This time of year is the \"tale of two snowpacks.\" On the solar side, the mornings are crusty, but this crust melts rapidly in the April sun. Today the top 5cm of the snow was moist by midday making for sticky ski conditions and increasing avalanche hazard. On the polar aspects, the snowpack is more wintery in nature with wind slabs in lee and cross-loaded terrain in the Alpine and wind prone areas at Treeline. Recent human and naturally-triggered avalanches on northerly aspects indicate that wind slabs are still a concern. Cornices are also large and looming and deserve respect, especially in the blazing sun.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8qep5","text":"The current thaw which will continue on Wednesday is causing a significant decrease in the level of snowpackl in the mountains. Our observations at mid-mountain are 25cm of snow on the ground. We have no other observations higher up in altitude for the moment but expect to find a thin snow cover over rocks and shrubs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8qep5","text":"The current thaw which is ending tonight cause a significant decrease in the level of the snowpack. Our mid station reported less than 15 cm of snow on the ground today. We have no other observations higher up in altitude for the moment but expect to find a frozen thin snow cover over rocks and shrubs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8qep5","text":"Following the heavy rain episode (60-100 mm) and warm spell (+10C at 1145m), the snowpack is almost entirely gone. Our mid-station  (635 m) reported around 20 cm on the ground today while no snow is found in the valley. We have no other observations higher up in altitude for the moment but expect to find a frozen and thin snow cover over rocks and shrubs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8qep5","text":"It has been cold and dry since the last warm spell (heavy rain episode with 60-100 mm of rain and +10C temperatures). Therefore, the snowpack is very thin and icy. Our mid-station (635 m) reported around 20 cm on the ground today while the valley floor is back to bare ground. We have no other observations higher up in altitude for the moment but expect to find a frozen and thin snowpack barely covering rocks and shrubs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"8qep5","text":"Dust of snow has fallen yesterday. Our mid-station (635 m) reported around 25 cm on the ground today while the valley floor is back to bare ground. We have no other observations higher up in altitude for the moment but expect to find a frozen and thin snowpack barely covering rocks and shrubs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"bc5t8","text":"About 5 to 10 cm of snow has fallen since the beginning of the storm. Our mid-station (635 m) is now reporting around 35 cm on the ground while 5 cm of snow is barely covering the ground in the valley. We have no other observations higher up in elevation for the moment but expect to find about 15 to 25 cm of new snow above a melt-freeze crust and barely covered rocks and shrubs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}
{"blocks":[{"key":"bc5t8","text":"Approximately 5 to 10 cm of snow fell with the weekend storm. Our mid-station (635 m) is still reporting around 35 cm on the ground while barely 5 cm of snow covers the ground in the valley. Our observations at higher elevation remain limited for the moment but expect to find a thin layer of new snow above a meltfreeze crust and barely covered rocks and shrubs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{}}