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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity has diminished since an avalanche cycle up to at least size 3 occurred in this region over the weekend, ending on Tuesday. There were a few close calls during this cycle. On Sunday in the Hankin area, a skier accidentally triggered a size 2.5 avalanche which resulted in a full burial and minor injuries. The avalanche was reported to have occurred on a wind-loaded, north-facing slope. The avalanche initially failed on the January crust/surface hoar combo, and then stepped-down to the November crust and basal facets. On the same day in the Sinclair area, a snowmobile may have been the trigger for a size 3 avalanche. The avalanche had a crown between 1 and 2 metres, and propagated up to 200 metres wide. It occurred on a wind-loaded, north-facing alpine slope and may have failed on the November crust facet combo. On Tuesday 27th, a couple of small skier-triggered avalanches were reported. One occurred on a steep roll over at lower treeline elevation and ran on the mid-January layer. The other was a small section of wind slab that pulled off a ridge line in wind affected terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A series of alarming large remotely-triggered avalanches was reported over the last few days. On Wednesday, a size 3 slab was observed on an east aspect at 2200 m. This may have been remotely triggered by a skier. It started in the upper (January) persistent weak layer and stepped down to the deeper (December) weakness. On Tuesday, two persistent slabs up to size 2.5 were triggered remotely in the alpine. There was also a natural size 3.5 avalanche on an east aspect that was estimated to be about 200 cm deep and may also have been the mid-December layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A large size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) yesterday on the December weak layer. Although that area is in the South Rockies, there have been similar snowpack characteristics observed in parts of this region, for example near the Corbin (Heartbreak/ Rain Gauge) areas. Over the past 4 days there have been numerous loose wet and wet slab avalanches up to size 2.5 releasing naturally, mostly on solar affected aspects. The forecast cooling trend should result in a decrease of natural activity; however solar aspects on Friday may still be a concern during the warmest parts of the day. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days, a widespread natural avalanche cycle took place to size 3.5 in response to loading from heavy precipitation, wind and warm temperatures. Many avalanches failed within the recent storm snow, although numerous avalanches also failed on persistent and deep persistent layers. Most of the avalanche activity had subsided by Tuesday 27th, although human triggered avalanches were reported to size 2 and explosive controlled avalanches were reported to size 2.5. With forecast snow and wind, I expect ongoing storm slab activity, and the potential for deep destructive persistent slab avalanches remains.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">As the temperature continues to drops I expect that avalanche activity will slow down. The recent snow, rain, and wind were a great test of buried persistent weaknesses in the snowpack and resulted in a widespread avalanche cycle. The mid-January surface hoar layer was responsible for the majority of the recent avalanche activity although there have been reports from the Selkirks of occasional releases to ground and on the mid-December layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">There was a widespread avalanche cycle earlier in the week in response to the warm storm, with a round of persistent slabs. Natural activity has now eased, but a few cornice drops triggered storm slabs on Thursday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">There was a widespread avalanche cycle earlier in the week in response to the warm storm. Natural activity has now eased, but explosives were able to trigger several large slabs (some failing sympathetically with each other) up to size 3 on the January surface hoar layer on Thursday around 2200 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">There are no new reports of avalanches. The large (size 3.5) natural avalanche reported earlier in the week from the SE aspect of Mt Ymir was found to have released on the mid-December DPWL (deep persistent weak layer) rather than the mid-January PWL (persistent weak layer) that we initially thought was the sliding layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. On Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December PWL.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There were a few close calls last weekend and into Tuesday. On Sunday in the Hankin area, a skier accidentally triggered a size 2.5 avalanche which resulted in a full burial and minor injuries. The avalanche was reported to have occurred on a wind-loaded, north-facing slope. The avalanche initially failed on the January crust/surface hoar combo, and then stepped-down to the November crust and basal facets. On the same day in the Sinclair area, a snowmobile may have been the trigger for a size 3 avalanche. The avalanche had a crown between 1 and 2 metres, and propagated up to 200 metres wide. It occurred on a wind-loaded, north-facing alpine slope and may have failed on the November crust facet combo. On Tuesday 27th, a couple of small skier-triggered avalanches were reported. One occurred on a steep roll over at lower treeline elevation and ran on the mid-January layer. The other was a small section of wind slab that pulled off a ridge line in wind affected terrain. In the wake storm loading on Friday, I would expect ongoing storm slab activity (especially in wind-exposed terrain) with the potential to trigger deeper, more destructive persistent layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A series of alarming large remotely-triggered avalanches was reported this week. On Wednesday, a size 3 slab was observed on an east aspect at 2200 m. This may have been remotely triggered by a skier. It started in the upper (January) persistent weak layer and stepped down to the deeper (December) weakness. On Tuesday, two persistent slabs up to size 2.5 were triggered remotely in the alpine. There was also a natural size 3.5 avalanche on an east aspect that was estimated to be about 200 cm deep and may also have been the mid-December layer. Explosives also triggered a size 2.5 slab on Thursday which failed on surface hoar over a metre deep.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches reported. On Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December PWL. Although that area is in the South Rockies region, there have been similar snowpack characteristics observed in parts of this region, for example near the Corbin (Heartbreak/ Rain Gauge) areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">At the time of publishing this bulletin, there was no new avalanche activity reported from the field. That said, I'm sure there was a healthy round of storm slab activity in response to heavy snow accumulations on Friday. Looking forward, I'd remain cautious of recently formed storm slabs, as they may remain sensitive to human triggering, especially in wind-exposed terrain. Additionally, persistent weak layers should remain on your radar as they may become reactive with the loading of the new snow, or with warming and solar radiation forecast for Saturday. Any avalanche on these deeper persistent weaknesses would be destructive in nature.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">There was a widespread avalanche cycle earlier in the week in response to the warm storm. Natural activity has now eased, but isolated slabs to size 3 were still observed on Thursday, failing on buried persistent weak layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches reported. I would expect a round of wind slab activity with new snow and wind forecast for Sunday</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There was a widespread avalanche cycle earlier in the week that produced numerous large to very large avalanches. Natural activity has now eased, but the present of persistent layers in snow pack suggest that it may be possible for humans to trigger an avalanche</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">There was a widespread avalanche cycle earlier in the week in response to the warm storm. Natural activity has now eased, but explosives were able to trigger several large slabs (some failing sympathetically with each other) up to size 3 on the January surface hoar layer on Thursday around 2200 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_C70F60E9">No new avalanches have been reported. On Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December persistent weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous small loose dry avalanches were seen today. Most of them were in steep, cliff terrain and didn't run as far as expected. There was one notable slab avalanche: Sz 2, E asp, 2200m alpine start zone, steep rocky terrain and a re-loaded bed surface from the last cycle.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several storm slabs to size 2.5 were reported in the wake of Thursday night's storm. With more snow and wind on the way on Sunday, I'd expect continued storm slab activity. It's important to keep in mind, a surface avalanche in motion may be what it takes to trigger deeper, more destructive persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There was a widespread avalanche cycle earlier in the week that produced numerous large to very large avalanches. Natural activity has now eased, but the present of persistent layers in snow pack suggest that it may be possible for humans to trigger an avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_FA956E1D">On Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December persistent weak layer. Although that area is technically in the South Rockies region, there have been similar snowpack characteristics observed in parts of this region, for example near the Corbin (Heartbreak/ Rain Gauge) areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. If snow accumulations are significant on Sunday, there may be a round of wind slab activity in high elevation terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several storm slabs to size 2.5 were reported in the wake of Thursday night's storm. With more snow and wind on the way on Sunday, I'd expect continued storm slab activity. It's important to keep in mind, a surface avalanche in motion may be what it takes to trigger deeper, more destructive persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555"> Natural activity has now eased after last weeks pineapple express but isolated large to very large slab avalanches were observed on Thursday, failing on buried persistent weak layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">At the time of publishing this bulletin, no new avalanches had been reported. That said, I'm sure thin wind slabs may have been easily triggered in response to Sunday's weather. With more snow on the way, I expect continued wind slab activity in lee terrain at treeline and above.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There was a widespread avalanche cycle earlier in the week that produced numerous large to very large avalanches. Natural activity has now eased, but the present of persistent layers in snow pack suggest that it may be possible for humans to trigger an avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There was a widespread avalanche cycle earlier in the week that produced numerous large to very large avalanches. Natural activity has now eased, but the present of persistent layers in snow pack suggest that it may be possible for humans to trigger an avalanche. Forecast snow above a crust and SH means a reactive soft slab is likely to form.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_C70F60E9">No new avalanches have been reported. On Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December persistent weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanche activity was observed. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several storm slabs to size 2.5 were reported in the wake of Thursday night's storm. With more snow and wind on the way on Sunday night and Monday, I'd expect continued storm slab activity. It's important to keep in mind, a surface avalanche in motion may be what it takes to trigger deeper, more destructive persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There was a widespread avalanche cycle earlier in the week that produced numerous large to very large avalanches. Natural activity has now eased, but the present of persistent layers in snow pack suggest that it may be possible for humans to trigger an avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_FA956E1D">On Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December persistent weak layer. Although that area is technically in the South Rockies region, there have been similar snowpack characteristics observed in parts of this region, for example near the Corbin (Heartbreak/ Rain Gauge) areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">At the time of publishing this bulletin, no new avalanches had been reported. That said, I'm sure there was a good round of wind slab activity in response to Sunday's weather. With more snow on the way, I expect continued wind slab activity in lee terrain at treeline and above.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several storm slabs to size 2.5 were reported in the wake of Thursday night's storm. With more snow and wind on the way on Sunday, I'd expect continued storm slab activity. It's important to keep in mind, a surface avalanche in motion may be what it takes to trigger deeper, more destructive persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There was a widespread avalanche cycle last week that produced numerous large to very large avalanches. Natural activity has now eased, but the present of persistent layers in snow pack suggest that it may be possible for humans to trigger an avalanche. Forecast snow above a crust and SH means a thin reactive soft slab is likely to form.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, small soft wind slabs were reported to be reactive to skier triggering.  Observations from the region have been limited but conditions are expected to be similar to the Sea-to-Sky where skier-triggered and explosive-triggered avalanches have been limited to size 1 and isolated to wind-loaded features.&nbsp; </span><span class="s_3FE45715">Similar conditions are expected on Tuesday with natural avalanches not expected and skier-triggered avalanches remaining possible in wind-loaded features.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> No new avalanches reported on Sunday. I expect that the new storm snow may have been easy to trigger where it was overlying a crust and/or surface hoar that was buried on January 30th. The new storm snow is likely to settle into a soft slab over the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some soft slab storm snow avalanches were reported on Sunday. I suspect that new storm snow avalanches were easy to trigger on Monday where the new snow was sitting on a hard crust and/or surface hoar that developed during the recent clear weather. Expect avalanche size to increase with incremental loading of the new storm slab later this week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. Last Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December persistent weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing from the last 24hrs, but there is a fair bit of older action from open areas at treeline and immediate lee areas at lower the alpine elevations. Sz2's were spotted mostly on the south &amp; south east aspects. The eastern side of the road also had some recent activity in the alpine. Most involved the basal layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new slab avalanches were reported on Sunday but sluffing from steep terrain was.&nbsp; On Saturday, a skier triggered a size 1 which released down 20-30cm.&nbsp; Natural activity up to size 3 was reported on Thursday and Friday during and following the storm.&nbsp; </span><span class="s_3FE45715">Skier triggering remains a concern for Monday but natural avalanches are generally not expected. Wind loaded features are my biggest concern for triggering but thin-spot triggering of persistent weakness would have the biggest consequences.&nbsp; Small avalanches also have the potential to step-down to a deeper weakness.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. I suspect that the new storm snow may not bond well to the old crust and/or surface hoar, resulting in easy triggering of a thin soft slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday a size 2 avalanche was accidentally triggered on an east aspect in the alpine by a sledder near Racehorse Pass (Crowsnest) on the December persistent weak layer. Although that area is technically in the South Rockies region, there have been similar snowpack characteristics observed in parts of this region, for example near the Corbin (Heartbreak/ Rain Gauge) areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On both Sunday and Monday, ski-cutting and explosives were producing thin soft slabs which were running on the firm crust layer. These were limited to size 1 and were isolated to wind affected terrain. Sluffing from steep terrain features was also reported. Similar conditions are expected on Tuesday with natural avalanches not expected and skier-triggered avalanches remaining possible in wind-loaded features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Sunday.  On Saturday, a skier triggered a size 1 which released down 25cm.  Natural avalanches to size 2.5 were reported on Thursday and Friday during and after the storm.  Skier triggering remains a concern for Monday but natural avalanches are generally not expected.  Wind loaded features are my biggest concern for triggering but thin-spot triggering of persistent weakness would have the biggest consequences. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> No new avalanches reported on Sunday. I expect the new storm snow may be easy to trigger where it overlays a hard crust and/or surface hoar. Incremental loading may increase the size of avalanches as the storm slab develops.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, skiers were triggering soft wind slabs in immediately leeward features up to size 2. On Sunday, small soft wind slabs were reported to be reactive to skier triggering. Sluffing from steep terrain features was also reported. Similar conditions are expected on Wednesday with natural avalanches not expected and skier-triggered avalanches remaining possible in wind-loaded features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There were numerous small size 1.0 Loose dry and soft storm slab avalanches releasing at the storm snow/crust interface, or pockets of wind transported snow at ridgetops.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There were numerous size 1.0 natural and skier triggered avalanches, and explosives triggered avalanches up to size 2.0 reported on Monday. In some areas pockets of wind transported snow were easy to trigger at ridgetops where they were sitting on a hard crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">New avalanche activity has been limited to minor sluffing in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanches were seen today</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, natural and human-triggered avalanches size 1 to 1.5 were reported in the south of the region. These were 20-30cm thick in sheltered areas and 30cm+ in wind loaded features. Sluffing from steep terrain was also reported. On Wednesday, natural avalanches are possible on sun exposed slopes or recently wind-loaded features. Skier-triggering is likely in wind loaded features and areas where the recent snowfall is settling into a cohesive slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several size 1.0 natural avalanches released in the new storm snow on Monday. On Tuesday there was a size 1.5 skier accidental near Golden with three people involved that may have released on the mid-January persistent weak layer on an East aspect in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday thin (15cm) storm slabs ran to size 2 on N and NE facing slopes between 1700 &amp; 1900m, running on the crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On both Sunday and Monday, ski-cutting and explosives were producing thin soft slabs which were running on the firm crust layer. These were limited to size 1 and were isolated to wind affected terrain. Sluffing from steep terrain features was also reported. Similar conditions are expected on Wednesday with natural avalanches not expected and skier-triggered avalanches remaining possible in wind-loaded features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, skiers triggered a few size 1 to 1.5 storm slabs.&nbsp; The size 1.5 avalanche released 40cm deep on a NE aspect at 1200m elevation. Sluffing from steep terrain was also reported. Some natural activity was reported on Monday in the NW Inland region. On Wednesday, natural avalanches are possible on sun exposed slopes or recently wind-loaded features. Skier-triggering is likely in wind loaded features and areas where the recent snowfall is settling into a cohesive slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose snow and storm slab avalanches released naturally and were skier triggered up to size 1.5 on Monday. I suspect the soft slab is settling and becoming more cohesive, allowing for longer propagations. Pockets of wind transported snow at ridgetops may be easy to trigger where they are sitting on a hard crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported Tuesday. On Monday, skiers were triggering soft wind slabs in immediately leeward features up to size 2. On Sunday, small soft wind slabs were reported to be reactive to skier triggering. Sluffing from steep terrain features was also reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There were a couple of natural cornice falls up to size 2.5 over the past few days, and several thin soft slab or loose snow avalanches up to size 1.0. The new storm starting on Thursday is expected to develop a thick storm slab that may release naturally and also may step down to the mid-January persistent weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There were numerous size 1.5 natural and skier triggered avalanches reported from Tuesday. In some areas pockets of wind transported snow were easy to trigger up to size 1.5 at ridgetops where they were sitting on a hard crust. I suspect continued loading from the forecast snow and wind over the next few days may result in widespread natural activity within the storm slab, or on the crust that was buried at the end of January. Storm slab avalanches in motion may result in persistent weak layer avalanches which may be large and destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">New avalanche activity includes skier and explosive controlled wind slab avalanches up to Size 2, as well as an accidentally triggered 30cm thick persistent slab avalanche that ran on the mid-December buried surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> No new avalanche reported today. Expect avalanches to be easily triggered and possibly some natural activity as the snow keeps accumulating during the day tomorrow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was one sz2 noted today on an alpine feature. It was approx 2300m, and an east aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Small wind slabs near ridge crest were reported Tuesday to size 1.  On Monday, natural and human-triggered avalanches size 1 to 1.5 were reported in the south of the region. These were 20-30cm thick in sheltered areas and 30cm+ in wind loaded features. Sluffing from steep terrain was also reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several natural and skier controlled avalanches up to size 1.5 mostly on North or Northeast aspects. There were a couple of remotely triggered avalanches up to size 2.0 that released down about 40 cm above the end of January crust. There was one skier accidental size 2.0 (reported yesterday as size 1.5) on a Northeast aspect in the alpine that released down 40-60 cm on the mid-January surface hoar (3.0 mm).</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> No new avalanche reported today. Expect avalanches to be easily triggered and possibly some natural activity as the snow keeps accumulating during the day tomorrow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday skiers intentionally initiated a few small slabs on small steep features. Activity on both Sunday and Monday was limited to ski-cutting and explosives induced thin soft slabs which were running on the firm crust layer. These were limited to size 1 and were isolated to wind affected terrain. Sluffing from steep terrain features was also reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday and Tuesday wind and storm slab avalanches to size 1.5 ran both naturally and with human provocation. Sluffing from steep terrain was also reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A size 2.5 natural avalanche in the Selkirks released from a steep North aspect in the alpine on the January 30th buried crust. Several smaller avalanches released naturally or were ski-cut that released within the storm slab or on the January 30th crust in the Monashees and the Selkirks. Storm slab avalanches are expected to release naturally and increase in size and frequency over the next few days as the storm intensifies and freezing levels climb. Storm slab avalanches in motion may step down to the mid-January persistent weak layer that is buried close to a metre in may areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant avalanche activity to report form Wednesday. I suspect that there should be plenty to report from Thursday, assuming there's enough visibility to see!</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There were a couple of size 1.0 storm slab avalanches on Wednesday that were triggered by skiers. The storm slab was reported to have settled into a more cohesive slab with the warming temperatures. Expect natural avalanche activity and avalanche size to increase with storm loading.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several natural avalanches up to size 2.0 were reported on Wednesday that released within the storm snow down 20-30 cm. Heavy loading from new snow and wind on Thursday is expected to have resulted in a storm slab cycle on the late January crust or on a change within the storm snow about 10-15 cm above the crust. Forecast strong winds and heavy snow are expected to increase avalanche size and avalanche frequency as the storm continues.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Multiple natural and skier triggered avalanches up to size 2.5 were reported within the storm snow some of which had impressive propagation potential. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> Several skier and explosive triggered avalanches up to size 2 out of treeline and alpine start zones were reported. Sluffing and shooting cracks were also observed as a slab was developing in the afternoon. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No activity was noted today due to limited visibility.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A number of size 1 to 2 avalanches in the recent storm snow were reported Wednesday.&nbsp; Small wind slabs near ridge crest were reported Tuesday to size 1. On Monday, natural and human-triggered avalanches size 1 to 1.5 were reported in the south of the region. These were 20-30cm thick in sheltered areas and 30cm+ in wind loaded features. Sluffing from steep terrain was also reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural and skier controlled avalanches up to size 1.5 were reported from Wednesday that released down about 40 cm on the late January crust. First reports from Thursday are that a very touchy storm slab 25 cm deep developed that was easy to trigger by ski-cutting. Expect a widespread natural avalanche cycle to result from the forecast strong winds and heavy snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> Several skier, explosive and snowmobile triggered avalanches up to size 2 were reported today at treeline and below treeline.&nbsp; There was limited visibility in the alpine making it difficult to observe, however, I suspect that some natural avalanches occurred.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant avalanche activity to report form Wednesday. I suspect that there should be plenty to report from Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, (before the storm) a size 2.5 wind slab avalanche was reported from a steep SE facing feature at 1300m. I suspect there will be more activity to report on in the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several avalanches size 1.0 were reported from Wednesday that were releasing down 20-30 cm within the storm snow. Preliminary reports from Thursday are that a storm snow cycle started today with the heavy loading from new snow and wind. Expect avalanche activity and avalanche size to increase as the storm continues to develop the storm slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday we received reports of avalanches running to size 3 both naturally and with explosive control work on all aspects in the northern portion of the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Thursday due to limited observations during the storm. There were a couple of size 1.0 storm slab avalanches on Wednesday that were triggered by skiers. The storm slab was reported to have settled into a more cohesive slab with the warming temperatures. Expect natural avalanche activity and avalanche size to increase with storm loading.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural avalanche activity up to size 2.0 was reported from the Selkirks and Monashees where slab avalanches released within the storm snow on Thursday. Observations were limited due to poor visibility and travel conditions on Friday</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A natural slab and loose avalanche cycle up to size 2.5 within the new snow started on Thursday afternoon. I suspect that avalanche conditions were similar on Friday even though poor visibility did not allow for good observations.&nbsp; </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> Natural and skier triggered moist and wet slab avalanches up to size 2 were reported on Friday in the alpine and at treeline. These would have failed within the storm snow. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Visibility was limited throughout the day on Friday but a few new slides were observed and reported into the forecasting office.  Of note was a sz 2.5 Na in the Buller Mountain control zone.  This run was skied a few days ago and today slid to ground down 1.5m in some places.  This was on a NE aspect at 2200m in 30-40deg terrain and 70m wide. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">With the intense storm obscuring views, observations have been limited. I expect there is a widespread natural avalanche cycle occurring, we'll probably learn more about it as skies clear this weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural and explosive controlled avalanches up to size 2.5 reported releasing in the storm snow. I suspect that there was a widespread natural avalanche cycle on Friday. Limited reports due to poor visibility and limited travel.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">2 natural slab avalanches size 3 and multiple explosive triggered avalanches up to size 3 were reported Friday out of the alpine/treeline from north, northeast and east aspects. These avalanches released within the storm snow. There was limited observation and visibility Friday but I suspect the natural avalanche cycle that started Thursday kept going on Friday. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday we received reports of avalanches running to size 3 both naturally and with explosive control work on all aspects. There were also reports of cornice fall triggering large avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">I suspect large natural avalanches are running Friday, but we do not have any observations at the moment.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural avalanches released within the storm snow up to size 2.5 in both the Monashees and Selkirks on Thursday. There were also a couple of very large avalanches in the Selkirks that we have limited information about due to poor visibility.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday we received reports of avalanches running to size 3 both naturally and with explosive control work on all aspects at and above treeline in the northern portion of the region. Loose wet avalanches were intentionally triggered to size 1.5 at and below treeline. In the south a natural cycle of loose wet avalanches to size 2 was observed on steep headwall features. Several glide avalanches to size 2 were also observed from steep rock features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations from the Cariboos have been limited during the storm but several natural size 2 storm slabs were observed on Friday. In the North Columbia region, natural avalanches up to size 3.5 were reported on Saturday. On Sunday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Sunday. If the sun comes out on Sunday, solar aspects will likely see natural avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3.5 were reported on Friday and Saturday. On Sunday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Sunday. If the sun comes out on Sunday, solar aspects will likely see natural avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the last few days there was a widespread natural avalanche cycle to size 3. Most of the avalanches were storm slabs which formed in response to new snow and wind. At lower elevations, a couple of wet slabs to size 3 were observed. With forecast weather storm slab avalanches will remain a concern with the potential to step down to deeper persistent layers. Loose wet and wet slab avalanches will also remain likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been extremely limited in recent days. That said, several storm slab avalanches to size 2.5 were reported in the south of the region on Friday. I get the feeling this was just the tip of the iceberg. Triggering storm slabs will remain a concern at higher elevations for the next few days. At lower elevations where precipitation has fallen as rain, I would expect ongoing loose wet and wet slab avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural avalanches were observed throughout the day on Saturday.  Many of these slides were sz 1.5-2 and failing within the storm snow but there were also a few larger slides, likely triggerred by Cornice failures that were failing down deeper in the snowpack producing size 3 avalanches.  Most of these slides initiated in Alpine terrain and ran to the middle of their normal runouts. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">I suspect large natural avalanches were running Friday, but we do not have any observations from treeline/alpine elevations where the action is at.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural, human-triggered, and explosive controlled avalanches up to size 2.5 were reported on Friday. This activity is expected to have continued on Saturday. On Sunday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Sunday. If the sun comes out on Sunday, solar aspects will likely see natural avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, there was a widespread storm slab avalanche cycle to size 3 in the Lizard Range. Due to inclement weather, observations elsewhere in the region were very limited. At higher elevations, storm slab triggering will remain a concern, especially due to the persistent nature of the buried crust/surface hoar interface. At lower elevations, continued warming should promote ongoing loose wet and wet slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosive control work Saturday produced storm slab avalanches to size 3 running 50 to 80cm in depth on the early February crust. Natural loose wet avalanches were reported to have run in the last 48 hours to size 2 as high as 2150m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">I suspect large natural avalanches were running Friday, but we do not have any observations from treeline/alpine elevations where the action is at.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3.5 were reported on Friday and Saturday. On Sunday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Sunday. If the sun comes out on Sunday, solar aspects will likely see natural avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">At the height of the storm in the northern portion of the region avalanches ran to size 3 on the February 1st Crust. Wet avalanches below 1950m were also observed. In the southern portion of the region several small glide avalanche releases were observed on rock slabs below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural cycle to size 3.5 has been reported between Friday and Sunday. This includes both storm slabs and persistent slabs. Avalanches are expected to be starting dry and ending wet, potentially running to valley bottom. On Monday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday and Saturday. This includes both storm slabs and persistent slabs. </span><span class="s_3FE45715">Many avalanches started dry and ended wet, running to valley bottom. </span><span class="s_3FE45715">On Monday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Monday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the last few days there was a widespread natural avalanche cycle to size 3. Most of the avalanches were storm slabs which formed in response to new snow and wind. At lower elevations, a couple of wet slabs to size 3 were observed. With forecast weather storm slab avalanches will remain a concern with the potential to step down to deeper persistent layers. Loose wet and wet slab avalanches will also remain likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several storm slab avalanches to size 2.5 were reported in the south of the region on Friday. On Saturday, storm slab avalanches to size 2 were also noted. I get the feeling this was just the tip of the iceberg as observations were extremely limited. Triggering storm slabs will remain a concern at higher elevations for the next few days. At lower elevations where precipitation has fallen as rain, I would expect ongoing loose wet and wet slab avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were confirmed today, however there were too many fresh crowns to rule out the end of the natural cycle. Public photo submissions yesterday informed us of significant avalanches at Burstall Pass. A sz2,5 was remotely triggered near a windloaded alpine feature. In Hero's Bowl, some paths went to valley bottom.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday we received observations of the recent storm cycle which featured natural avalanches to size 3. The details are a bit fuzzy, but it sounds like most of this activity was limited to mid-storm instabilities. There is a good video of ski cut easily triggering a slab avalanche in seemingly benign terrain on the Bulkley Backcountry Ski Society facebook page too.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday and Saturday. This includes both storm slabs and persistent slabs.  Many avalanches started dry and ended wet, running to valley bottom.  On Sunday, a skier was involved in an accident in the Canyon Creek area.&nbsp; The subject was caught in a size 2.5 persistent slab which resulted in serious injuries. The avalanche released on the mid-January surface hoar layer down around 80cm. On Monday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Monday.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday and Saturday, there was a widespread storm slab avalanche cycle to size 3 in the Lizard Range. On Saturday there was also a report of a size 3.5 natural loose wet avalanche. On Sunday, similar avalanche activity was observed with wet slabs to size 3 thrown into the mix. Due to inclement weather, observations elsewhere in the region were very limited. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">With more snow and wind forecast for Monday, storm slab triggering will remain a concern, especially due to the persistent nature of the buried crust/surface hoar interface. At lower elevations, continued warming should promote ongoing loose wet and wet slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosive control work Saturday produced storm slab avalanches to size 3 running 50 to 150cm in depth on the early February crust. Natural loose wet avalanches were reported to have run in the last 48 hours to size 2 as high as 2150m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Scanning the facebook posts it sounds like at least two folks were involved in avalanches Saturday.  Control work Saturday produced slab and loose dry avalanches to size 2.5 from virtually all aspects and elevations. It sounds like a lot of these were running on mid storm instabilities.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3.5 were reported on Friday and Saturday. This includes both storm slabs and persistent slabs. Many avalanches started dry and ended wet, running to valley bottom. On Monday, natural avalanches remain likely at upper elevations where storm and wind loading continue. At lower elevations which have seen rain, natural activity is less likely but remains possible. Human-triggering remains very likely at higher elevations on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday avalanche activity was limited to pin wheeling from solar aspects. At the height of the storm in the northern portion of the region avalanches ran to size 3 on the early February crust. Wet avalanches below 1950m were also observed. In the southern portion of the region several small glide avalanche releases were observed on rock slabs below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural cycle to size 3.5 has been reported on Friday through Sunday. This includes both storm slabs and persistent slabs. Avalanches are expected to be starting dry and ending wet, potentially running to valley bottom. </span><span class="s_3FE45715">On Tuesday, natural avalanches remain possible at upper elevations but are generally not expected. Human-triggering remains likely and travel in avalanche terrain is not recommended until the storm slab has had a chance to stabilize.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday through Sunday. This includes both storm slabs and persistent slabs. Many avalanches started dry and ended wet, running to valley bottom. On Tuesday, natural avalanches remain possible at upper elevations but are generally not expected. Human-triggering remains likely and travel in avalanche terrain is not recommended until the storm slab has had a chance to stabilize.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the last few days there was a widespread avalanche cycle to size 3.5. Most of the avalanches were storm slabs which formed in response to new snow and wind, although many avalanches stepped down to the late and mid January surface hoar/crust layers. On Sunday, many of these avalanches were still failing naturally or with remote triggers. Looking forward, very large persistent slab avalanches remain a concern, especially with forecast warm temperatures and potential for solar radiation.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">At lower elevations where the snowpack is rain-soaked, there is potential for ongoing loose wet or wet slab avalanches. Although if snow surfaces refreeze and form a strong crust, this will be unlikely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations have been essentially non-existent in recent days. This likely speaks more to a lack of observers rather than actual conditions. I'm confident recent storm loading has produced large storm slab avalanches at higher elevations, while loose wet or wet slab avalanche activity occurred at lower elevations where rain fell.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanches observed today, but visibility was quite limited. Ski cutting produces small slabs in steep terrain at Treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend we received limited observations of the recent storm cycle which featured natural avalanches to size 4. The details are a bit fuzzy, but it sounds like most of this activity was limited to mid-storm instabilities. I suspect that some of the bigger ones likely stepped down to deeper instabilities, but that's all conjecture. There is a good video of ski cut easily triggering a slab avalanche in seemingly benign terrain on the Bulkley Backcountry Ski Society facebook page too.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday through Sunday. This includes both storm slabs and persistent slabs. Many avalanches started dry and ended wet, running to valley bottom. On Sunday, a skier was involved in an accident in the Canyon Creek area. The subject was caught in a size 2.5 persistent slab which resulted in serious injuries. The avalanche released on the mid-January surface hoar layer down around 80cm. On Tuesday, natural avalanches remain possible at upper elevations but are generally not expected. Human-triggering remains likely and travel in avalanche terrain is not recommended until the storm slab has had a chance to stabilize. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days there was a widespread storm slab avalanche cycle to size 3. Many of the storm slab avalanches failed on the late January curst/surface hoar combo. At elevations where rain fell, loose wet and wet slabs to size 3.5 were also noted. Large storm slab avalanches will remain a concern, especially due to the persistent nature of the buried crust/surface hoar interface. At lower elevations where the snowpack is rain-soaked, there is potential for ongoing loose wet or wet slab avalanches. Although if snow surfaces refreeze and form a strong crust, this will be unlikely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Control work on Sunday produced storm slabs to size 2.5 with crown depths of 50 to 150cm. This is a slight reduction in size from Saturday's control work that produced storm slab avalanches to size 3 running 50 to 150cm in depth on the early February crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No significant activity to report from Sunday. Scanning the facebook posts it sounds like at least two folks were involved in avalanches Saturday. Control work Saturday produced slab and loose dry avalanches to size 2.5 from virtually all aspects and elevations. It sounds like a lot of these were running on mid storm instabilities.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3.5 were reported on Friday through Sunday. This includes both storm slabs and persistent slabs. Many avalanches started dry and ended wet, running to valley bottom. On Tuesday, natural avalanches remain possible at upper elevations but are generally not expected. Human-triggering remains likely and travel in avalanche terrain is not recommended until the storm slab has had a chance to stabilize.</span></p>
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</style><p class="p_CC664AAA"><span class="s_7D940460">Avalanche activity over the last couple of days was limited to loose wet avalanches on steep solar aspects. At the height of the storm in the northern portion of the region avalanches ran to size 3 on the early February crust. Wet avalanches below 1950m were also observed. In the southern portion of the region several small glide avalanche releases were observed on rock slabs below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday through Monday during the storm. This includes both storm slabs and persistent slabs. On Wednesday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the storm slab remains possible, especially on steep slopes and wind loaded features in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday through Monday during the storm. This includes both storm slabs and persistent slabs. On Wednesday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the storm slab remains possible, especially on steep slopes and wind loaded features in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations have been essentially non-existent in recent days. This likely speaks more to a lack of observers rather than actual conditions. I'm confident recent storm loading has produced large storm slab avalanches at higher elevations, while loose wet or wet slab avalanche activity occurred at lower elevations where rain fell.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations have been essentially non-existent in recent days. This likely speaks more to a lack of observers rather than actual conditions. I'm confident recent storm loading has produced large storm slab avalanches at higher elevations, while loose wet or wet slab avalanche activity occurred at lower elevations where rain fell.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A significant natural avalanche cycle has occurred over the last 4 days. Some ski-triggered slides have also been reported. Activity has tapered off, but 2 new naturally triggered slabs were observed today on E aspects between 2300 and 2600m. These slabs were both size 2.0 and appeared to be storm snow slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no recent reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We haven't received any repots of new avalanches in the last couple of days and over the weekend we received only a few observations. It sounds like most of the weekends avalanche activity was limited to mid-storm instabilities although at least one ran on the early February surface hoar. I suspect that some of the bigger ones likely stepped down to deeper week layers, but thats just a guess.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday through Monday. This includes storm slabs and persistent slabs. On Sunday, a skier was involved in an accident in the Canyon Creek area. The subject was caught in a size 2.5 persistent slab which resulted in serious injuries. The avalanche released on the mid-January surface hoar layer down around 80cm. On Tuesday, explosive triggered a size 2.5 avalanche on the November crust/facet layer. This occurred in an area that had previously slide and then reloaded. On Wednesday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the storm slab remains possible, especially on steep slopes and wind loaded features in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days there was a widespread storm slab avalanche cycle to size 3. Many of the storm slab avalanches failed on the late January curst/surface hoar combo. At elevations where rain fell, loose wet and wet slabs to size 3.5 were also noted. Large storm slab avalanches will remain a concern, especially due to the persistent nature of the buried crust/surface hoar interface. At lower elevations where the snowpack is rain-soaked, there is potential for ongoing loose wet or wet slab avalanches. Although if snow surfaces refreeze and form a strong crust, this will be unlikely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity appears to have tapered off for now although small lose wet avalanches have been reported in steep terrain.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose natural avalanches are being reported from steep terrain. While natural slab avalanches appear to becoming less frequent avalanche control on Monday produced slab avalanches up to size 3 on virtually all aspects and elevations. It sounds like a lot of these avalanches ran on mid storm instabilities although some larger results observed on South facing slopes released on the late January crust. Glide cracks were reported from the Shames backcountry on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural, human-triggered, and explosive controlled avalanches up to size 3 were reported on Friday through Monday during the storm. This includes both storm slabs and persistent slabs. On Wednesday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the storm slab remains possible, especially on steep slopes and wind loaded features in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Slab avalanche activity appears to have tapered off for now although small lose wet avalanches have been reported in steep terrain at lower elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread avalanche cycle occurred on Friday through Monday during the storm. Activity has tapered off on Tuesday. The only report is of explosives triggering a size 3 avalanche with a slab depth of 200cm. In the North Columbia region, isolated natural activity was reported on Tuesday. On Thursday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the persistent slab remains possible, especially on steep slopes and wind loaded features in the alpine. If new wind slabs form overnight Wednesday, they may be touchy on Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread avalanche cycle occurred on Friday through Monday during the storm. Activity tapered off on Tuesday but isolated natural avalanches to size 2.5 were reported. Explosives also produced slab avalanches and loose wet results. On Thursday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the persistent slab remains possible, especially on steep slopes and wind loaded features in the alpine. If new wind slabs form overnight Wednesday, they may be touchy on Thursday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports from Tuesday include evidence of old natural slab avalanches up to Size 2.5. Heavy triggers such as explosives and snowcats were able to trigger 20-90 cm deep storm slabs up to Size 2, but no new naturals were observed and ski-cutting was ineffective.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations have been essentially non-existent in recent days. This likely speaks more to a lack of observers rather than actual conditions. I'm confident recent storm loading has produced large storm slab avalanches at higher elevations, while loose wet or wet slab avalanche activity occurred at lower elevations where rain fell.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Avalanches aren't expected at this time.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Warming temperatures, wind, snow and rain are will drive a natural avalanche cycle that I expect to last the next couple of days. Activity over the weekend was mainly limited to short lived storm instabilities although at least one avalanche released on the early February surface hoar.&nbsp; I suspect that some of the bigger ones that were reported may have stepped down to even deeper week layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread avalanche cycle occurred on Friday through Monday during the storm. Natural activity tapered off on Tuesday but human-triggered and explosive-triggered avalanches to size 3 were reported.&nbsp; A skier triggered a persistent slab avalanche on the mid-Jan layer in the Dogtooth range and went for a ride. Explosives triggered several avalanches on the late-Jan layer and one skier remote was reported on the same layer.&nbsp; Explosives also triggered a size 2.5 avalanche on the November crust/facet layer in an area that had previously slide and then reloaded. On Thursday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the persistent slab remains possible, especially on steep slopes and wind loaded features in the alpine. If new wind slabs form overnight Wednesday, they may be touchy on Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday include an isolated natural Size 2.5 avalanches with moist powerful debris. Large explosives produced minimal results at treeline elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity appears to have tapered off for now although small lose wet avalanches have been reported in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Warming temperatures, wind, snow and rain will drive a natural avalanche cycle that I expect to last the next couple of days. Avalanche control on Monday produced slab avalanches up to size 3 on virtually all aspects and elevations. It sounds like a lot of these avalanches ran on mid storm instabilities although some larger results observed on South facing slopes released on the late January crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread avalanche cycle occurred on Friday through Monday during the storm. Activity tapered off on Tuesday but isolated natural avalanches to size 2.5 were reported. Natural loose wet activity has also been reported from sun exposed rocky features. Explosives produced slab avalanches to size 2.5. On Thursday, natural activity is generally not expected but is possible on steep south-facing slopes if the sun comes out. Human-triggering of the persistent slab remains possible, especially on steep slopes and wind loaded features in the alpine. If new wind slabs form overnight Wednesday, they may be touchy on Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">This is a test bulletin</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche have been reported recently although I expect wind slabs could be reactive in the high alpine and loose wet avalanche are probably still popping off bellow the freezing level and on steep alpine slopes that see brief periods of sun.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">No new avalanches were reported on Wednesday. On Tuesday, explosives triggered a size 3 avalanche with a slab depth of 200cm. A widespread avalanche cycle occurred on Friday through Monday during the storm. Human-triggering of the persistent slab and/or wind slabs remains possible. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Loose wet avalanches to size 2 were triggered naturally and by skiers on Wednesday. These occurred on steep faces that caught some sun and at low elevations where the snowpack is water-soaked. A size 2.5 persistent slab failed on a steep shallow rocky feature at 2500 m, approximately 1 m deep. Cornices also collapsed naturally and with explosives.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only one size 1 skier controlled avalanche on a steep convex roll was reported on Wednesday. Reports from Tuesday include evidence of old natural slab avalanches up to Size 2.5. Heavy triggers such as explosives and snowcats were able to trigger 20-90 cm deep storm slabs up to Size 2, but no new naturals were observed and ski-cutting was ineffective.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations have been essentially non-existent in recent days. This likely speaks more to a lack of observers rather than actual conditions. I'm confident recent storm loading has produced large storm slab avalanches at higher elevations, while loose wet or wet slab avalanche activity occurred at lower elevations where rain fell.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches today</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche have been reported yet through this storm    At least one one avalanche last weekend on the early February surface hoar and I suspect that some of the bigger ones that were reported may have stepped down to even deeper week layers.  Given the uncertainty I would keep these layers in mind especially in areas that receive more snowfall through this system.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Natural avalanche activity has been tapering since last weekend's storm cycle, but skiers and explosives were still producing large avalanches on Wednesday: A skier triggered a size 2 persistent slab avalanche on the mid-Jan layer in the Dogtooth range and went for a ride. Explosives also triggered a size 3 slab which started with a cornice failure, then ripped out to ground. Explosives triggered a size 2.5 avalanche on the November crust/facet layer in an area that had previously slid and then reloaded. A very large natural slab was also observed just outside the region near Invermere (look for the blue pin on the bulletin regions map to get the full report). Clearly the snowpack is still capable of producing destructive avalanches, so tread carefully.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Thursday produced several large size 2-3 slab avalanches from steep start zones between 1800-2100 m. Many of these slides failed on or stepped down to deeply buried persistent weaknesses - possibly even layers that formed in November. There is still potential for large loads (like a cornice fall) to trigger isolated deep slabs in higher terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity appears to have tapered off for now although small lose wet avalanches have been reported in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Warming temperatures, wind, snow and rain are driving a natural avalanche cycle that started on Wednesday when we received reports of several natural and explosive controlled avalanches up to size 2 on wind loaded north-facing slopes. Avalanche control on Monday produced slab avalanches up to size 3 on virtually all aspects and elevations. It sounds like some these avalanches released on the late January crust and I wouldn't be surprised if we continue to see activity on this layer over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Loose wet avalanches failed naturally in steep terrain on Wednesday in response to warming. Explosives triggered large cornices and a couple of size 2 slabs, which failed on the late-Jan crust. </span><span class="s_3D0464D1">Human-triggering of the persistent slab remains possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Avalanche activity appears to have tapered off for now although small lose wet avalanches have been reported in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Size 1.5 wind slabs and a size 2.5 storm slab were triggered naturally on Thursday. A number of cornice collapses have been reported over the last few days. Loose wet avalanches failed naturally in steep terrain on Wednesday in response to warming. Also on Wednesday, explosives triggered a couple of size 2 slabs, which failed on the late-Jan crust. Human-triggering of the persistent slab remains possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Skiers triggered a very large (size 3.5) persistent slab on Thursday on a NE aspect in the alpine in the Monashees. It failed on the late-Jan layer. Several large avalanches also failed naturally. Some failed in the recent storm snow, and some were glide crack releases and wet slabs gouging to ground. On Wednesday, a size 2.5 persistent slab failed on a steep shallow rocky feature at 2500 m, approximately 1 m deep. Cornices also collapsed naturally and with explosives over the last couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports from Thursday include isolated large explosive triggered persistent slab avalanches failing on the mid-January surface hoar on northeast facing treeline and alpine slopes. These slabs were 80-150 cm thick with some wind-loaded pockets as deep as 2 m. One avalanche was described as 'sluggish', but highly destructive, taking out mature timber on the way down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports from Thursday include two cornice-triggered that stepped down to a deep persistent slab on a hanging face. A couple of explosive-triggered storm and and wind slabs up to Size 2 were also reported, but ski-cutting produced no results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A bombing mission on Rundle had limited results. 3 of the 4 bombs produced avalanches up to sz2. All of them failed on the Jan31st layer. Previous control had dealt with the deeper layers, so these results are not necessarily transferable to the backcountry.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We haven't received any new avalanche reports recently but that may just be because not many people are getting out. Given the uncertainty I would keep keep the persistent week layers in mind over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">On Thursday, a size 2 natural avalanche was observed on a north-facing slope. Explosives also triggered numerous size 2-3.5 avalanches up to 2 m deep, some of which ran at ground. Large cornice falls were also observed. On Wednesday, a skier took a ride in a size 2 persistent slab which failed on the mid-Jan layer in the Dogtooth range. Explosives also triggered a size 3 slab which started with a cornice failure, then ripped out to ground. Explosives triggered a size 2.5 avalanche on the November crust/facet layer in an area that had previously slid and then reloaded. A very large natural slab was also observed just outside the region near Invermere (look for the blue pin on the bulletin regions map to get the full report). Clearly the snowpack is still capable of producing destructive avalanches, so tread carefully.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Thursday produced several large size 2-3 slab avalanches from steep start zones between 1800-2100 m. Many of these slides failed on or stepped down to deeply buried persistent weaknesses - possibly even layers that formed in November. There is still potential for large loads (like a cornice fall) to trigger isolated deep slabs in higher terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche have been reported recently although I expect thin wind slabs could be reactive in the high alpine and loose wet avalanche are probably still popping on steep alpine slopes that see brief periods of sun.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Warm temperatures, wind, snow and rain drove a natural avalanche cycle that started on Wednesday.  Since then we have received reports of  numerous natural and explosive controlled slab avalanches up to size 3 on all aspects above 1000m with widespread loose wet avalanche activity bellow . I am unsure if all of these avalanche were contained to the storm snow or if some may have released on one o</span><span class="s_2488BF4F">f the deeper week layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Size 1.5 wind slabs and a size 2.5 storm slab were triggered naturally on Thursday. A number of cornice collapses have been reported over the last few days. Loose wet avalanches failed naturally in steep terrain on Wednesday in response to warming. Also on Wednesday, explosives triggered a couple of size 2 slabs, which failed on the late-Jan crust. Human-triggering of the persistent slab remains possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There has been recent loose wet avalanche activity reported from the Tenquille Lake area in the north of the region. I get the feeling this was just the tip of the iceberg given the ongoing warm temperatures. I expect thin wind slabs could be reactive in the high alpine and loose wet avalanche are probably still popping on steep alpine slopes that see brief periods of sun.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several size 1.5-2.5 avalanches were triggered naturally on Thursday and Friday in response to storm loading, wind and warm temperatures. </span><span class="s_3D0464D1">A number of cornice collapses have been reported over the last few days. Loose wet avalanches failed naturally in steep terrain on Wednesday in response to warming. Also on Wednesday, explosives triggered a couple of size 2 slabs, which failed on the late-Jan crust. Human-triggering of the persistent slab remains possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A warming-related natural avalanche cycle occurred on Thursday and Friday. Many cornices also collapsed naturally and with explosives over the last few days, occasionally triggering slabs on the slopes below. Skiers triggered a very large (size 3.5) persistent slab on Thursday on a NE aspect in the alpine in the Monashees. It failed on the late-Jan layer. Avalanche activity is likely to taper off with cooling temperatures, but large avalanches remain possible, and sun may cause another spike in avalanche activity on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports from Friday include natural loose wet and wet slab avlanches up to size 2.5. Reports from Thursday include isolated large explosive triggered persistent slab avalanches failing on the mid-January surface hoar on northeast facing treeline and alpine slopes. These slabs were 80-150 cm thick with some wind-loaded pockets as deep as 2 m. One avalanche was described as 'sluggish', but highly destructive, taking out mature timber on the way down.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations were seen on Saturday but field teams were out of the field by 13:00hrs.  Prior to this time, skies were obscured and visibility was limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet and wet slab avalanche activity to size 2.5 was observed in the last few days. If warm temperatures persist, there is ongoing potential for this type of activity to continue. Wind slabs to size 2 were also observed at higher elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A couple of large naturally-triggered slabs were observed on Friday in response to warming. One was a size 3 on a west aspect at around 2500 m. Size 2 avalanches were also observed on NE aspects. On Thursday, a size 2 natural avalanche was observed on a north-facing slope. Explosives also triggered numerous size 2-3.5 avalanches up to 2 m deep, some of which ran at ground. Large cornice falls were also observed. On Wednesday, a skier took a ride in a size 2 persistent slab which failed on the mid-Jan layer in the Dogtooth range. As temperatures cool this weekend, conditions should gradually improve, but large avalanches remain possible, and sun may cause another spike in avalanche activity on steep solar aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Thursday produced several large size 2-3 slab avalanches from steep start zones between 1800-2100 m. Many of these slides failed on or stepped down to deeply buried persistent weaknesses - possibly even layers that formed in November. There is still potential for large loads (like a cornice fall) to trigger isolated deep slabs in higher terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. I expect thin wind slab avalanches could be triggered in isolated high alpine terrain, although I would expect them to gain strength fairly quickly. With forecast warming, loose wet and wet slab avalanches will remain a concern, particularly on steeper, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Wet loose and wet slab avalanche activity to size 2.5 was observed in the south of the region in the last few days. If warm temperatures persist, there is ongoing potential for this type of activity to continue.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">On Friday, warm temperatures led to a loose wet avalanche cycle. Size 1.5 wind slabs and a size 2.5 storm slab were triggered naturally on Thursday. A number of cornice collapses have been reported over the last few days. Direct sun may spark a new avalanche cycle on steep slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Saturday. With continued warming, loose wet avalanches and cornice failures will remain the primary concern, particularly on steeper, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several size 1.5-2.5 avalanches were triggered naturally over the last few days in response to storm loading, wind and warm temperatures. A number of cornice collapses have been reported over the last few days. Now that temperatures have cooled, avalanche activity is likely to ease, although d</span><span class="s_3D0464D1">irect sun may spark a new avalanche cycle on steep slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several size 1.5-3 avalanches were triggered naturally over the last few days in response to storm loading, wind and warm temperatures. A number of cornice collapses and an ice fall have also been reported. </span><span class="s_3D0464D1">Skiers triggered a very large (size 3.5) persistent slab on Thursday on a NE aspect in the alpine in the Monashees. It failed on the late-Jan layer. </span><span class="s_1681A555">Now that temperatures have cooled, avalanche activity is likely to ease, although d</span><span class="s_3D0464D1">irect sun may spark a new avalanche cycle on steep slopes or cause more cornices to fall.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday there was one loose wet avalanche size 2.0 that released from a steep northeast aspect at treeline. I suspect that cooler alpine temperatures and the re-freezing has reduced the likelihood of triggering deeply buried weak layers. Some loose wet avalanche activity may continue if we see strong solar radiation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier accidental sz 2.5 avalanche occurred late in the day on Saturday.  The slide occurred on an E aspect at 2400m, was 130m wide, up to 100cm deep and ran over 600m.  5 skiers were involved and one fatality resulted.  Yesterday several sz 2-3 avalanches were observed when the sun came out.  Some of the fracture lines were over 500m wide failing at what appeared to be the jan 31st interface down 50-90cm and some avalanches also stepped down to ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday, loose wet avalanche activity to size 2.5 was observed. With forecast warming and solar radiation, I would expect ongoing loose wet activity with the potential for wet slab avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several size 1.5-3 avalanches were triggered naturally and with explosives over the last few days in response to storm loading, wind and warm temperatures. A number of cornice collapses and an ice fall have also been reported. Last</span><span class="s_3D0464D1"> Wednesday, a skier took a ride in a size 2 persistent slab which failed on the mid-Jan layer in the Dogtooth range. </span><span class="s_1681A555">Now that temperatures have cooled, avalanche activity is likely to ease, although d</span><span class="s_3D0464D1">irect sun may spark a new avalanche cycle on steep slopes or cause cornices to fail.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There were a couple of small loose wet avalanches reported that were a result of ski-cutting below treeline. I suspect that the overnight re-freeze down to valley bottoms has developed a new surface crust and will reduce the likelihood of triggering deeply buried weak layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A size 2 storm slab was observed on Saturday. It likely formed in response to new snow and wind on Friday With continued warming, loose wet avalanches and cornice failures will remain the primary concern, particularly on steeper, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosives control produced storm slabs to size 2 on Saturday in the far north of the region. Otherwise, no new avalanches were reported. With forecast warming and solar radiation, I would expect a round of loose wet avalanche activity with potential for cornice falls and wet slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several size 1.5-3 avalanches were triggered naturally over the last few days in response to storm loading, wind and warm temperatures. A number of cornice collapses and an ice fall have also been reported. Now that temperatures have cooled, avalanche activity is likely to ease, although d</span><span class="s_3D0464D1">irect sun may spark avalanche activity on steep slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">With continued warming, loose wet avalanches and cornice failures will remain the primary concern, particularly on steeper, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports from Sunday include one explosive-triggered cornice fall (that did not trigger a slab) and one explosive-triggered loose snow sluff from steep unsupported terrain. There was more evidence of the previous natural avalanche cycle with numerous slides up to size 3. </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity tapered off on Sunday as temperatures cooled but conditions allowed for good viewing of the natural avalanche cycle from the previous few days. Many observers reported natural and cornice triggered slabs, typically size 1.5-3 with a few up to size 3.5. Sunshine may spark a new avalanche cycle on steep slopes (mainly loose wet) or cause more cornices to fall.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports from Sunday are limited to small wet loose snow activity on steep sun-exposed slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There are many avalanches out there at the moment. A very large natural avalanche was noted today on Mt. Worthington. Sz3.5, 2700m, SE aspect, 50 degree slope, 1.5m deep by 500m wide. Unknown trigger.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. With forecast warming and solar radiation on Tuesday, I would expect a round of loose wet avalanche activity with potential for cornice falls and wet slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches were observed on Sunday. However, there were a few more reports of previous activity with slabs up to size 3. Sunshine and daytime warming could trigger loose wet sluffs, cornice collapses, and isolated deeper slabs this week. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Sunday or Monday morning.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">With continued warming, loose wet avalanches and cornice failures will remain the primary concern, particularly on steeper, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. With forecast warming and solar radiation on Tuesday, I would expect a round of loose wet avalanche activity with potential for cornice falls and wet slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Several size 1 skier-controlled wind slabs and a few natural cornice triggered slabs to size 2 were reported on Sunday. There were also reports of two size 3 natural slabs from south facing slopes in the high alpine (likely solar triggered). Sunshine and daytime warming could continue to trigger loose wet sluffs, isolated slabs and cause cornice failures. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches were reported within the Cariboos on Monday, but neighboring regions reported thin skier-triggered wind slabs to size 1, small loose sluffs, and a few natural and explosive triggered slabs and cornice falls to size 3. </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Explosive control work on Monday produced a few size 2-3 slab avalanches. Most of these were from steep alpine slopes and the majority were on southerly aspects. There were also a couple reports of natural and explosive triggered cornice falls, some of which triggered slabs up to size 2 (one stepped down to the November crust). This recent activity suggests that conditions have improved, but large loads (like a cornice fall) could still trigger deeper persistent weaknesses, primarily in alpine terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported on Monday or Tuesday morning.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some small, loose dry avalanches from yesterday were noted today. No slab avalanches were seen.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. There will likely be a shift to new wind slab activity with snow and wind forecast for late Wednesday.</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_17AE1194">A couple natural slab avalanches up to size 2.5 were observed or reported on Monday. There were also a few explosive triggered slabs and cornice falls (some of which then triggered slabs) up to size 3. All activity was from very steep, high alpine terrain on a variety of aspects. </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_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Monday or Tuesday morning.</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_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported.</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">Explosives control produced storm slab avalanches to size 2 in the far north of the region on Monday. Otherwise, no new avalanches have been reported. There will likely be a shift to new wind slab activity with snow and wind forecast for late Wednesday.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Several thin size 1 skier-triggered wind slabs and natural loose snow avalanches were reported on Monday. There were also a couple reports of natural cornice falls triggering slabs up to size three, and there was one report of a size 2.5 avalanche that was triggered remotely by a helicopter landing on a ridge. </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_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. Small wind slab avalanches may form in response to light snowfall and strong winds on Thursday.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday a couple natural cornice falls were observed. These were size 2-2.5 but did not trigger slabs on the slopes below. There was also one report of a size 3 slab on a sun-exposed alpine slope. This slide was observed from a distance but did look fresh. Neighboring regions reported similar activity with cornice fall and isolated deep slabs being the main concern. </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_17AE1194">For the past few days we have seen a few size 2-3 natural and explosive triggered slabs and cornice failures (sometimes triggering slabs and sometimes not) each day. Almost all of these have been from steep alpine terrain on a variety of aspects. On Tuesday there were also a few reports of loose wet slides from very steep south-facing slopes in the alpine. </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">Things appear to be locked up tight and no new avalanches have been reported in the last couple of days.</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">No new avalanches have been reported recently</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">No new avalanches</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">Sometime during the last few days, a natural cornice fall triggered a large slab avalanche in steep, rocky alpine terrain near Smithers. (see the latest Mountain Information Network post for pictures and more details) Loose wet avalanches to size 1.5 were also noted on Tuesday in response to warming and solar radiation. There will likely be a shift to new wind slab activity with snow and wind forecast for Thursday.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Early this week there were several reports of natural and explosive triggered slabs and cornice falls to size 3. Almost all of these slides occurred on high alpine slopes with cornice related activity being specific to NE-E slopes below ridges. On Tuesday there were also reports of fresh wind slabs (10-20 cm thick) being reactive to skier traffic. </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; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches have been reported recently.</span><span class="s_3FE45715" /></p>
<style type="text/css">
.p_CC664AAA { margin: 0px 0px 12px 0px;text-align: left;text-indent: 0pt;padding: 0px 0px 0px 0px; } 
.s_3FE45715 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #000000; } 
</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. Small wind slab avalanches may occur in response to light snow and wind forecast for Thursday.</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">In the far north of the region on Tuesday, explosives avalanche control produced deep persistent slab avalanches to size 4 in the big terrain near Stewart. Otherwise, no new avalanches have been reported. There will likely be a shift to new wind slab activity with snow and wind forecast for late Wednesday.</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_17AE1194">Several thin size 1-1.5 skier-triggered wind slabs and natural loose snow avalanches were reported on Monday and Tuesday. There were also a couple reports of natural or explosive triggered cornice falls triggering slabs up to size three, and there was one report of a size 2.5 avalanche that was triggered remotely by a helicopter landing on a ridge on Monday. </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">Test:Hard and soft wind slabs in lee features to size 1.5</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 activity has been limited to small loose wet avalanches on steep sunny terrain features. </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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday and Wednesday a couple natural and explosive triggered cornice falls were reported. These were size 2-2.5 and some triggered slabs on the slopes below while others did not. Neighboring regions reported similar activity with cornice fall and isolated deep slabs being the main concern. </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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">For the past few days we have seen a few size 2-3 natural and explosive triggered slabs and cornice failures (sometimes triggering slabs and sometimes not) each day. Almost all of these have been from steep alpine terrain on a variety of aspects. There have also been reports of the odd small (size 1) skier triggered wind slab. </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">Things appear to be locked up tight and no new avalanches have been reported in the last couple of days.</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">No new avalanches have been reported recently</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">No new activity today.</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_69982360">Sometime during the last few days, a natural cornice fall triggered a large slab avalanche in steep, rocky alpine terrain near Smithers (see the latest Mountain Information Network post for pictures and more details). Loose wet avalanches to size 1.5 were also noted on Tuesday in response to warming and solar radiation. </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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Over the past several days there have been reports of natural and explosive triggered slabs and cornice falls to size 3. Almost all of these slides occurred on high alpine slopes with cornice related activity being specific to NE-E slopes below ridges. On Tuesday there were also reports of fresh wind slabs (10-20 cm thick) being reactive to skier traffic. </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_1681A555">No new avalanches have been reported recently.</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">No new avalanches have been reported.</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_69982360 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 15.3333333333333px;color: #5B5B5B; } 
</style><p class="p_CC664AAA"><span class="s_69982360">Most of the recent avalanche activity has been confined to the big terrain near Stewart. On Wednesday, a size 3 glide slab released and several loose wet avalanches were triggered by solar warming. On Tuesday, explosives avalanche control produced deep persistent slab avalanches to size 4. Elsewhere, there has been little reported.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Throughout the week there have been decreasing numbers of reports of natural and explosive triggered slabs and cornice falls, generally size 2 to 3. There have also been a few reports of size 1 skier triggered wind slabs in steep unsupported or cross-loaded terrain. All recent activity has been from higher alpine terrain. </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_3D0464D1">No new avalanches have been reported.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday there were a couple reports of natural cornice falls, but these did not trigger slabs. There was also a report of a size 1 (20 cm deep) skier controlled wind slab from an East facing slope. Wind slabs could build and remain sensitive to rider triggering throughout the weekend. </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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday there were a couple reports of natural cornice falls, but these did not trigger slabs. There were also a few reports of size 1 skier controlled wind slabs from East facing slopes. These were typically around 20 cm deep. Wind slabs could build and remain sensitive to rider triggering throughout the weekend. </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">Things appear to be locked up tight and no new avalanches have been reported in the last couple of days.</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">No new avalanches have been reported recently</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">Nothing new.</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; } 
.s_3D0464D1 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span><span class="s_3D0464D1">No new avalanches have been reported. Avalanche danger is expected to be lower in the cool parts of the day, and rise during warm, sunny periods. As temperatures rise, keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday explosive control work on steep North and East facing slopes only resulted in loose snow sluffs. Earlier in the week there were reports of natural and explosive triggered cornice falls and slabs, typically size 2-3 and all from alpine terrain. </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">No new avalanches have been reported recently.</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">No new avalanches have been reported.</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_3D0464D1 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Avalanche danger is expected to be lower in the cool parts of the day, and rise during warm, sunny periods. As temperatures rise, keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday there were a couple reports of natural cornice falls, but these did not trigger slabs. There were also a few reports of size 1 skier controlled wind slabs from East facing slopes. These were typically around 20 cm deep. Wind slabs could build and remain sensitive to rider triggering throughout the weekend. </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">No new avalanche activity has been reported</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_3D0464D1 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 14px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported.</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_17AE1194 { font-family: 'Arial';font-style: Normal;font-weight: normal;font-size: 13.3333333333333px;color: #121212; } 
</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday there were a couple reports of natural cornice falls, but these did not trigger slabs. There was also a report of a size 1 (20 cm deep) skier controlled wind slab from an East facing slope. Wind slabs could build and remain sensitive to rider triggering throughout the weekend. </span></p>
<style type="text/css">
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday there were a couple reports of natural cornice falls, but these did not trigger slabs. There were also a few reports of size 1 skier controlled wind slabs from East facing slopes. These were typically around 20 cm deep. Recently developed wind slabs could remain sensitive to rider triggering throughout the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Things appear to be locked up tight and no new avalanches have been reported in the last couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two size 2.0 naturally triggered slabs were observed today on steep SW aspects in the Alpine. These were only approximately 20cm deep but had wide propagations of over 100 metres. Very small loose dry slides were also observed in very steep Alpine terrain on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Naturally-triggered size 2 slabs were observed within recent storm snow in the north of the region. Cornices also failed on Friday. Avalanche danger is expected to be lower in the cool parts of the day, and rise during warm, sunny periods. As temperatures rise, also keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday explosive control work on steep North and East facing slopes only resulted in loose snow sluffs. Earlier in the week there were reports of natural and explosive triggered cornice falls and slabs, typically size 2-3 and all from alpine terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A cornice fall triggered a size 1 slab on Friday. Otherwise, no new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Several size 1-1.5 loose wet avalanches failed on steep sunny slopes yesterday. In the far north, two cornices collapsed and each triggered a size 3 slab on the slope below. Avalanche danger is expected to be lower in the cool parts of the day, and rise during warm, sunny periods. As temperatures rise, also keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the week. On Thursday there were a couple reports of natural cornice falls, but these did not trigger slabs. There were also a few reports of size 1 skier controlled wind slabs from East facing slopes. These were typically around 20 cm deep. With continued northeast winds, wind slabs could build and remain sensitive to rider triggering throughout the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the past week, although there may have been some wind slab activity at higher elevations over the weekend in response to northwest winds redistributing recent snow accumulations. Looking forward, wind slabs may remain sensitive to human triggering, while loose wet avalanches may fail under sunny skies and rising freezing levels.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the past week, although there has been some wind slab activity to size 1.5 at higher elevations over the weekend in response to northwest to northeast winds redistributing recent snow accumulations. Looking forward, wind slabs may remain sensitive to human triggering, while loose wet avalanches may fail under sunny skies and rising freezing levels on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity to report.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> There were numerous skier initiated sluffs in steep(&gt;40) terrain, but the sluffs were not running far and slowed to where the angle eased to 35deg. or less.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Naturally-triggered size 2 slabs were observed within recent storm snow in the north of the region. Cornices also failed on Friday. Avalanche danger is expected to be lower in the cool parts of the day, and rise during warm, sunny periods. As temperatures rise, also keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Last week there were reports of natural and explosive triggered cornice falls and slabs, typically size 2-3 and all from alpine terrain. Avalanche activity of this nature has gradually tapered off throughout the week. Looking forward, thin wind slabs may still be sensitive to triggering in high elevation terrain. Warming forecast for Monday may spark some loose wet avalanche activity on sun-exposed slopes while increasing the likelihood of deeper persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A cornice fall triggered a size 1 slab on Friday. Otherwise, no new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Small loose wet avalanches have been failing on steep sunny slopes. Skiers triggered small thin wind slabs on Saturday. In the far north, two cornices collapsed on Friday and each triggered a size 3 slab on the slope below. Avalanche danger is expected to be lower in the cool parts of the day, and rise during warm, sunny periods. As temperatures rise, keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has gradually tapered off throughout the past week, although there has been some wind slab activity to size 2 at higher elevations over the weekend in response to northwest to northeast winds redistributing recent snow accumulations. Looking forward, wind slabs may remain sensitive to human triggering, while loose wet avalanches may fail under sunny skies and rising freezing levels on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity has generally tapered off throughout the past week, although there was some reported human-triggered wind slab activity to size 1 at higher elevations over the last few days. The wind slabs formed in response to northwest winds redistributing recent snow accumulations. Current wind slabs may remain sensitive to human triggering while forecast strong northwest winds may promote new wind slab activity on south-facing slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Sunday a size 2 natural cornice fall was reported from the region. Also, wind slabs to size 1.5 were reported to have been triggered over the last few days on high elevation south-facing terrain. Current wind slabs may remain sensitive to human triggering while forecast strong northwest winds may promote new wind slab activity on south-facing slopes</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated small wind slabs on north aspects were reported Sunday, no other significant avalanche activity to report.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few isolated loose wet avalanches were noted today. All were about sz1.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Reports from Sunday include a few wet loose sluffs up to Size 2 from steep rocky sun-exposed terrain. A large cornice failure was also reported, but didn't trigger a slab on the slope below. Keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Over the last few days reported avalanche activity was limited to cornice falls from ridge crests in high elevation terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Small loose avalanches from steep alpine headwalls were reported Sunday.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported on Sunday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Reports from Sunday include Isolated wet releases up to Size 2.5 out of steep sun-exposed slopes, and pin wheeling on steep slopes at treeline and below. One large cornice failure was reported, but it didn't trigger any slabs on the slope below. As temperatures rise, keep in mind the possibility of glide slabs releasing on smooth rock surfaces - avoid traveling on or under slopes sporting glide cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Sunday a size 2.5 natural cornice fall was reported from 2500m in the northern Selkirks. Also, wind slabs to size 2 were reported to have been triggered over the last few days on high elevation south-facing terrain. Current wind slabs may remain sensitive to human triggering while forecast strong northwest winds may promote new wind slab activity on south-facing slopes</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several sluffs/loose snow avalanches to size 1.5 were observed from steep SW and W facing features during afternoon warming over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Reports from Monday include a few wet loose sluffs from steep sun-exposed rocky terrain, which was surprisingly little activity considering the high temperatures and solar radiation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday, several loose wet avalanches to size 2 occurred on sun-exposed slopes. We also received a report of a size 2.5 deep persistent avalanche which was triggered by a cornice fall. With a general cooling pattern forecast for the next few days, I would expect avalanche activity of this nature to taper-off.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">With the warm temperatures on Monday, fairly widespread loose wet avalanche activity to size 2 was observed in sun-exposed terrain. Under the warm skies, a size 3 glide crack avalanche was also observed. In the North Columbia region, there was also some persistent slab avalanche activity on sun-exposed alpine slopes to size 3.5. With the forecast cooling trend, avalanche activity of this nature should taper-off.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was reported on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural cornice sz 2.5, 2600m, NE aspect, initiated in steep cliffs and entrained snow below. There was widespread pin wheeling and loose wet avalanches from yesterday afternoon's heat. Average size was 1, with a few scattered 1.5's.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Reports from Monday include numerous wet releases up to Size 2 out of steep sun-exposed slopes. Isolated cornice failures were reported, but no slabs were triggered on the slopes below. Several recent full-depth glide avalanches up to Size 3 were also observed nearby on all but North aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Under Monday's warm skies, loose wet avalanches to size 2 were observed in sun-exposed terrain. That said, observations were limited, and the warming may have had a more widespread effect. In the neighboring North Columbia region, warming and solar radiation triggered some persistent slab avalanches to size 3.5. Forecast cooling should limit avalanche activity of this nature.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Small loose avalanches from steep alpine headwalls were reported Sunday. No new activity to report from Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Reports from Monday include numerous wet releases up to Size 2 out of steep sun-exposed slopes. Isolated cornice failures were reported, but no slabs were triggered on the slopes below. Several recent full-depth glide avalanches up to Size 3 were also observed on all but North aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday the region saw fairly widespread loose wet avalanche activity to size 2 on sun-exposed slopes. In some cases, solar warming triggered persistent slab avalanches to size 2.5 on the mid-January surface hoar layer in south-facing alpine terrain. In an isolated event in the Selkirks, solar warming triggered a slab on the mid-January weakness. The avalanche stepped down to a deeper weakness resulting in a size 3.5 slab avalanche. With forecast cooling, avalanche activity of this nature is expected to taper-off.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some small solar-triggered activity was reported on Monday and no new avalanches have been reported since.  Avalanche activity is generally not expected for Thursday except potentially isolated human-triggered wind slab activity if we get more snow than forecast Wednesday overnight.</span><span class="s_3D0464D1" /></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday, several loose wet avalanches to size 2 occurred on sun-exposed slopes. We also received a report of a size 2.5 deep persistent avalanche which was triggered by a cornice fall. With a general cooling pattern forecast for the next few days, I would expect avalanche activity of this nature to taper-off.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">With the warm temperatures on Monday, fairly widespread loose wet avalanche activity to size 2 was observed in sun-exposed terrain. Under the warm skies, a size 3 glide crack avalanche was also observed. In the North Columbia region, there was also some persistent slab avalanche activity on sun-exposed alpine slopes to size 3.5. With the forecast cooling trend, avalanche activity of this nature should taper-off.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was reported on Tuesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations today. Obscured skies for most of the day.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Tuesday. On Monday, numerous wet releases up to Size 2 were reported from steep sun-exposed slopes. Isolated cornice failures and ice falls have recently been reported. Last week several full-depth avalanches up to Size 3 were observed on all but North aspects. On Thursday, fresh wind slabs are the main concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Under Monday's warm skies, loose wet avalanches to size 2 were observed in sun-exposed terrain. That said, observations were limited, and the warming may have had a more widespread effect. In the neighboring North Columbia region, warming and solar radiation triggered some persistent slab avalanches to size 3.5. Forecast cooling should limit avalanche activity of this nature.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Small loose avalanches from steep alpine headwalls were reported Sunday. No new activity to report from Monday or Tuesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some small solar-triggered activity was reported on Monday and no new avalanches have been reported since. Avalanche activity is generally not expected for Thursday except potentially isolated human-triggered wind slab activity if we get more snow than forecast Wednesday overnight.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday, an explosive-triggered size 1 wind slab avalanche was reported.  On Monday, numerous wet releases up to Size 2 were reported from steep sun-exposed slopes. Isolated cornice failures and ice falls have recently been reported. Last week several full-depth avalanches up to Size 3 were observed on all but North aspects.  On Thursday, fresh wind slabs are the main concern.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday the region saw fairly widespread loose wet avalanche activity to size 2 on sun-exposed slopes. In some cases, solar warming triggered persistent slab avalanches to size 2.5 on the mid-January surface hoar layer in south-facing alpine terrain. In an isolated event in the Selkirks, solar warming triggered a slab on the mid-January weakness. The avalanche stepped down to a deeper layer resulting in a size 3.5 slab avalanche. With forecast cooling, avalanche activity of this nature is expected to taper-off.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some small solar-triggered activity was reported on Monday and no new avalanches have been reported since. Avalanches are generally not expected on Friday but could be possible on steep south-facing slopes if we get more sun than expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Wednesday there was a natural size 2.5 wind slab that released down 80 cm on a northwest aspect in the alpine. There was also a report of a natural cornice fall size 2.0 on a south aspect at 2600 metres.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity was reported on Tuesday or Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few small, isolated loose dry out of steep terrain. There was also a large natural cornice triggered avalanche above three isle lake within the past few days. This supports the large trigger idea when it comes to the deeper layers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported since Monday when numerous wet releases up to Size 2 were reported from steep sun-exposed slopes. Isolated cornice failures and ice falls have also recently been reported. Last week several full-depth avalanches up to Size 3 were observed on all but North aspects. As we get increased sun and warming heading into the weekend, these types of avalanches could once again become a problem.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Some moist loose snow avalanche up to size 2.0 were reported in the south of this region on Wednesday du to daytime heating from strong solar on steep south aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported this week. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some small solar-triggered activity was reported on Monday and no new avalanches have been reported since. Avalanches are generally not expected on Friday but could be possible on steep south-facing slopes if we get more sun than expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday, an explosive-triggered size 1 wind slab avalanche was reported. On Monday, numerous wet releases up to Size 2 were reported from steep sun-exposed slopes. Isolated cornice failures and ice falls were reported during the last sunny period. Last week several full-depth avalanches up to Size 3 were observed on all but North aspects. As we get increased sun and warming heading into the weekend, these types of avalanches could once again become a problem.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Wednesday there was a natural cornice fall that resulted in a size 2.0 avalanche, and did not release the slope that it fell on. Some explosives control resulted in cornices falling off up to size 2.5. There was also one skier accidental size 1.0 that released down 20 cm after about 30 people had skied the same slope.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. Avalanches are generally not expected on Saturday but small loose sluffing from steep sun exposed slopes is possible during the afternoon.  </span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported in the past few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No activity today</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some loose sluffing has been reported but no new avalanches. Avalanches are generally not expected on Saturday but small loose sluffing from steep sun exposed slopes is possible during the afternoon.  </span><span class="s_3FE45715">Last week several full-depth avalanches up to Size 3 were observed on all but North aspects. As we get increased sun and warming heading into the weekend, these types of large isolated avalanches could once again become a problem.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently. Avalanches are generally not expected on Saturday but small loose sluffing from steep sun exposed slopes is possible during the afternoon.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Thursday, several size 1 skier initiated avalanches were reported.  It is expected that these were thin wind slabs. Last week several full-depth avalanches up to Size 3 were observed on all but North aspects. If the region gets substantial warming and sun on Saturday, isolated events like these could once again become active.  Loose sluffs from steep sun exposed slopes are also possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Some natural cornice falls up to size 2.0 were reported on Thursday in the Selkirks. There was also a report of a skier accidentally triggering a size 1.0 windslab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">One size 2 avalanche was observed on February 26 on the east side of the White Pass. According to the observer it looked to be a couple days old and was likely triggered by a cornice fall. Check out the Mountain Information Network for a photo and more details. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported recently. Small loose wet avalanches are possible on sun-warmed slopes and it may be possible to trigger thin wind slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">A skier triggered a size 1.0 steep un-supported pocket of windslab on a northwest aspect at treeline in the Selkirks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported in the past few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Avalanches are generally unlikely, but small loose sluffing from steep sun exposed slopes is possible during warm parts of the day. Cornice fall and thin wind slabs may be triggered by people. Last week several full-depth avalanches up to size 3 were observed on all but north aspects. As we get increased sun and warming, these types of large isolated avalanches could once again become a problem.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">A small size 1.0 pocket of windslab was triggered accidentally by a skier on a northeast aspect in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Skiers triggered small size 1 wind slabs on Friday. More of the same is likely to be found as outflow winds continue. Small loose wet avalanches are possible on sun-warmed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">On Thursday and Friday, several size 1 skier initiated avalanches were reported. It is expected that these were thin wind slabs. Last week several full-depth avalanches up to size 3 were observed on all but north aspects. If the region gets substantial warming and sun again, isolated events like these could once again become active. Loose sluffs from steep sun exposed slopes are also possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">One natural cornice fall size 2.0 was reported on Friday in the Selkirks. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently. Small loose wet avalanches are possible on sun-warmed slopes and it may be possible to trigger thin wind slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Facetted surface snow has been reported to be sloughing in steep terrain. Isolated pockets of windslab have been reactive to skier triggering up to size 1.0.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported in the past few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently but observations are limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There were no new avalanches observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some cornice falls have been reported, but have not triggered slabs on slopes below. Last week, several full-depth avalanches up to size 3 were observed on all but north aspects. If the region gets substantial warming and sun again, isolated events like these could once again become active. Loose sluffs from steep sun exposed slopes are also possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Skiers triggered small size 1 wind slabs on Friday. More of the same is likely to be found as outflow winds continue. Small loose wet avalanches are possible on sun-warmed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday and Friday, several size 1 skier initiated avalanches were reported. It is expected that these were thin wind slabs. Some cornice falls have also been reported. Last week, several full-depth avalanches up to size 3 were observed on all but north aspects. If the region gets substantial warming and sun again, isolated events like these could once again become active. Loose sluffs from steep sun exposed slopes are also possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Some natural cornice falls size 2.0 were reported on Saturday in the Monashees and Selkirks. Also, a skier triggered a small size 1.0 pocket of wind slab on a north aspect in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported in the past few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently but observations are limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some older loose dry were noted today, but they were all small.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over the weekend avalanches to size 3 were reported from steep un-skiable south through west facing terrain features and isolated cornice fall produced a few slabs out of extreme terrain. Very thin wind slabs on NE facing alpine features were also observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier was involved in a small wind slab avalanche on a S/SE facing alpine feature on Saturday.  See more here:  http://bit.ly/1BQ4JtP  No other avalanche activity to report from the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 3 avalanche was observed from a steep un-skiable solar aspect over the weekend.&nbsp; Last week, several full-depth avalanches up to size 3 were observed on all but north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Some natural cornice falls size 2.0 were reported on Saturday in the Monashees and Selkirks. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On February 26, a size 2 slab avalanche was triggered by cornice fall on the east side of the White Pass (Big Blue drainage). Over the weekend, evidence of a deep, cornice-triggered slab avalanche (200m wide) was also noted on Cleveland Peak. The layers associated with these avalanches are unknown. Loose wet and wet slab avalanches to size 2.5 were also observed in steeper, sun-exposed terrain. These avalanches failed in response to last weekend's warming and solar radiation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported Saturday/Sunday/Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported. But neighbouring regions have been experiencing widespread dry loose sluffing in steep terrain and isolated small wind slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports from Monday and Tuesday morning include widespread dry loose sloughing up to Size 1.5 in steep terrain. Slope cutting also produced several Size 1 storm slabs and wind slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday there were reports of small rider-triggered loose snow avalanches in steep terrain. It might also be possible to trigger thin pockets of wind slabs in exposed lee terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently but observations are limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of solar induced sluffs were noted in steep rocky terrain. One avalanche of note occurred on Tent Ridge, in one of the gullies mid-ridge. It is estimated to be a size 2.5 which is large considering the lack of natural activity recently. Check out our Kananaskis Public Safety Facebook page for a picture of the Tent Ridge avalanche. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over the weekend avalanches to size 3 were reported from steep un-skiable south through west facing terrain features and isolated cornice fall produced a few slabs out of extreme terrain. Very thin wind slabs on NE facing alpine features were also observed. Glide cracks are starting to open up too.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports from Monday include several dry loose sluffs in steep terrain and thin soft wind slabs reacting to slope cuts with minimal propagation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A skier was involved in a small wind slab avalanche on a S/SE facing alpine feature on Saturday. See more here: http://bit.ly/1BQ4JtP No other avalanche activity to report from Saturday/Sunday/Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 3 avalanche was observed from a steep un-skiable solar aspect over the weekend. Several small wind slabs were observed on Monday. Last week, several full-depth avalanches up to size 3 were observed on all but north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports from Monday and Tuesday morning include widespread dry loose sloughing up to Size 1.5 in steep terrain. Slope cutting also produced several Size 1 storm slabs and wind slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">A skier remotely triggered a size 1.5 wind slab on Tuesday on a SE aspect in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported. But neighbouring regions have been experiencing widespread dry loose sluffing in steep terrain, and isolated small wind slab activity in exposed areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports Tuesday include widespread dry loose sloughing up to Size 1.5 in steep terrain. Slope cutting also produced isolated Size 1 wind slabs below ridge crests and on the leeward side of terrain features at treeline and above.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday there were reports of small wind slabs being triggered by explosives. Also, natural sun-triggered sluffing of the new snow was reported from steep sun-exposed slopes. On Thursday it should remain possible to trigger thin pockets of wind slabs in exposed leeward terrain features. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. Natural avalanches are generally not expected on Thursday but small human-triggered avalanches remain possible in isolated areas, specifically wind-loaded areas of the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches today</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A skier triggered an isolated size 1 wind slab in the alpine on Tuesday. Small loose moist avalanches were also observed on steep solar aspects over the last couple of days. Over the weekend, avalanches to size 3 were reported from steep un-skiable south through west facing terrain features and isolated cornice fall produced a few slabs out of extreme terrain. Very thin wind slabs on NE facing alpine features were also observed. Glide cracks are starting to open up too.</span><span class="s_1681A555"> New snow and wind are likely to create storm slabs and wind slabs which could be triggered naturally, or with the weight of a person.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports from Tuesday include several dry loose sluffs in steep terrain and thin soft wind slabs reacting to slope cuts with minimal propagation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently.&nbsp; Natural avalanches are generally not expected on Thursday but small human-triggered avalanches remain possible in isolated areas, specifically wind-loaded areas of the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">On Tuesday, a skier triggered a small size 1 hard wind slab in a cross-loaded terrain feature. A skier was involved in a small wind slab avalanche on a S/SE facing alpine feature on Saturday. See more here: http://bit.ly/1BQ4JtP. Otherwise there has been little avalanche activity over the last few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Small loose moist avalanches were observed on steep solar aspects over the last couple of days. Several small wind slabs were observed on Monday. A size 3 avalanche was observed from a steep un-skiable solar aspect over the weekend. Storm slabs and wind slabs are likely to form over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports Tuesday include widespread dry loose sloughing up to Size 1.5 in steep terrain. Slope cutting also produced isolated Size 1 wind slabs below ridge crests and on the leeward side of terrain features at treeline and above.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">A skier remotely triggered a size 1.5 wind slab on Tuesday on a SE aspect in the alpine. Otherwise there has been little recent avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">There was one new report of a size one skier-triggered wind slab on a steep convex roll on Wednesday. Neighbouring regions also experienced widespread dry loose sluffing in steep terrain, and isolated small wind slab activity in exposed areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Wednesday there were reports of several small (size 1-1.5) skier-triggered wind slab avalanches in exposed alpine terrain and loose snow sluffing in steep terrain. There were also two reports of size 2 natural slab avalanches on steep solar aspects, likely resulting from recent wind loading. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday and Wednesday there were reports of small wind slabs being triggered by skiers and explosives. Also, natural sun-triggered sluffing of the new snow was reported from steep sun-exposed slopes. On Friday it may remain possible to trigger thin pockets of wind slabs in exposed leeward terrain features. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. Natural avalanches are generally not expected on Friday but small human-triggered avalanches remain possible in isolated areas, specifically wind-loaded areas of the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">no activity today</span></p>
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</style><p class="p_CC664AAA"><span class="s_8BA0CF9D">Glide slabs have been releasing below treeline. </span><span class="s_A9A7295C">At the time of writing, no avalanches have been reported from Thursday, but there may have been some avalanche activity in response to snow and wind-loading.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Recent reports include several dry loose sluffs in steep terrain, and thin soft wind slabs reacting to slope cuts with minimal propagation. Explosive testing also resulted in one cornice fall that did not trigger a slab on the slope below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently. Natural avalanches are generally not expected on Friday but small human-triggered avalanches remain possible in isolated areas, specifically wind-loaded areas of the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A few size 1 wind slabs have been triggered by skiers this week. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">At the time of writing, no avalanches have been reported, but I expect a natural cycle occurred today in response to snow and wind-loading.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Wednesday there were several reports of small (size 1-1.5) skier-triggered wind slabs in exposed alpine terrain and loose snow sluffing in steep terrain. One observer reported seeing a couple natural size 2-2.5 slabs from steep solar aspects that were loaded by recent Northwest winds. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">On Friday a skier remotely triggered a size 1 (15cm deep) wind slab in the alpine. Otherwise there has been little recent avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small (size 1-1.5) skier-triggered wind slabs have been reported in exposed alpine terrain, and loose snow sluffing in steep terrain. One observer reported seeing a couple of natural size 2-2.5 slabs from steep solar aspects that were loaded by recent Northwest winds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Avalanche activity reports in the last few days have been confined to skier-triggered size 1 to 1.5 wind slabs in exposed alpine terrain and loose snow sluffing in steep terrain. . </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday and Wednesday there were reports of small wind slabs being triggered by skiers and explosives. Also, natural sun-triggered sluffing of the new snow was reported from steep sun-exposed slopes. As it warms and the amount of sun increases on Saturday, it may become easier to trigger the thin old pockets of wind slabs.&nbsp; During the afternoon it may be possible to trigger sluffing from steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. Natural avalanches are generally not expected on Saturday except possibly sun-triggered sluffing on steep south-facing slopes.  Human-triggered avalanches remain possible in isolated areas, specifically wind-loaded areas of the alpine or steep sun-exposed slopes.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some spindrift avalanches were seen this morning. Confined alpine gullies in the front ranges had small spindrift avalanches pouring down regularly.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">At the time of writing, no avalanches have been reported from Thursday, but there may have been some avalanche activity in response to recent snow and wind-loading.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Recent reports of loose sluffs in steep terrain, and thin soft wind slabs reacting to slope cuts with minimal propagation. Explosive testing also resulted in one cornice fall that did not trigger a slab on the slope below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently. Natural avalanches are generally not expected on Saturday except possibly sun-triggered sluffing on steep south-facing slopes.&nbsp; Human-triggered avalanches remain possible in isolated areas, specifically wind-loaded areas of the alpine or steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A few size 1 wind slabs have been triggered by skiers this week. No other avalanches have been observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">At the time of writing, observations were extremely limited, but I expect a large, widespread natural cycle occurred in response to snow and wind-loading over the past few days. I would expect ongoing potential for human triggering of the new snow due to underlying weak surfaces. Looking forward, I would expect natural storm slab activity to ramp up again with new snow and wind forecast for Sunday and Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">There have recently been several reports of small (size 1-1.5) skier-triggered wind slabs in exposed alpine terrain as well as loose snow sluffing in steep terrain. One observer reported seeing a couple of natural size 2-2.5 slabs from steep solar aspects that were loaded by recent Northwest winds. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Last weekend there was some large isolated avalanche activity that was related to warm temperatures and solar radiation. This included natural cornice failures which triggered slabs on the slopes below and loose wet/wet slab avalanches on steep sun-exposed slopes. No new avalanches were reported during the last week which was likely due to cooler temperatures and cloudy skies. A report from Friday suggests that the wind-affected new snow may be reactive to skiers but no new natural avalanches were observed. Over the weekend, isolated natural avalanches may be possible in steep, wind-loaded terrain features and thin wind slabs are expected to be reactive to human-triggers. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">On Friday a skier remotely triggered a size 1 (15cm deep) wind slab in the alpine. Otherwise there has been little recent avalanche activity. Forecast warming may increase the likelihood of cornice failures and loose wet avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small (size 1-1.5) skier-triggered wind slabs have been reported in exposed alpine terrain, and loose snow sluffing in steep terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Windslab avalanches up to size 1.5 were reported that were skier triggered near ridgetops in the Selkirks and Monashees.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday and Wednesday there were reports of small wind slabs being triggered by skiers and explosives. On Friday, natural sun-triggered sluffing was reported from steep sun-exposed slopes. As it warms and the amount of sun increases on Sunday, it may become easier to trigger the thin old pockets of wind slabs. During the afternoon it may be possible to trigger sluffing from steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, wet sluffing was reported from steep sun exposed slopes in the Lizard range. Similar conditions are expected on Sunday.  Human-triggering of old wind slabs also remains possible in isolated areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There have been no new reports of avalanche activity, although this may speak more to a lack of observations rather than actual conditions. I'm sure there was some recent wind slab activity in response to new snow and wind prior to the weekend. With more snow and wind forecast for Sunday and Monday, I would expect further wind slab activity, especially in areas to the west which are forecast to receive more snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Thin windslabs continue to be triggered up to size 1.5 near ridgetops in the alpine. One cornice failure was reported that released a pocket of windslab below that was 35 cm deep and size 1.5.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday, natural and skier triggered wet sluffing was reported from steep sun exposed slopes. Similar activity is expected on Sunday. Human-triggering of old wind slabs also remains possible in isolated areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Isolated size 1 wind slabs have been triggered by skiers as recently as Friday. No other avalanches have been observed. Forecast warming may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There was a surprisingly limited amount of reported natural avalanche activity given the amount of new snow and wind on Thursday and Friday. Size 1 soft slabs were reportedly sensitive to human triggering in high elevation lee terrain. That said, I'd remain cautious of steeper, high-consequence slopes as a release on recently buried surfaces could have nasty consequences. Looking forward, more wind and snow forecast for Sunday will likely spark a round of natural storm slab activity. New new snow will also add more stress to these recently buried weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">There have recently been several reports of small (size 1-1.5) skier-triggered wind slabs in exposed alpine terrain as well as loose snow sluffing in steep terrain. A snowmobile triggereda size 2.0 windslab on a northeast aspect at 1800 metres that was 20cm deep.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Forecast sunny skies may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was one report of a windslab size 2.0 that was 80 cm deep and released on a north aspect at 1900 metres. Forecast new snow and wind is expected to increase size and frequency of avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">One report of a large (possible size 3.0) avalanche in the Gold Range of the Monashees that was viewed from a distance with binoculars. This avalanche occurred in extreme terrain and is expected not to be cornice triggered. Warming temperatures this week and high freezing levels are a concern for persistent weak layers &quot;waking up.&quot;</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday and Wednesday there were reports of small wind slabs being triggered by skiers and explosives. On Friday, natural sun-triggered sluffing was reported from steep sun-exposed slopes. As warm conditions persist on Monday, it may still be possible to trigger old pockets of wind slabs. During the afternoon it may be possible to trigger sluffing from steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday in Kananaskis Country, a skier-trigger slab released on a weak layer near the ground. On Saturday, wet sluffing was reported from steep sun exposed slopes in the Lizard range.&nbsp;  Similar activity is still possible on Monday as the heat and sun continues.&nbsp; Human-triggering of old wind slabs also remains possible in isolated areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Report came in late yesterday of a skier triggered avalanche on the South face of Mt. Nestor, This was a size 2.0 that initiated at 2700m and ran well down into the track. This avalanche was a surface wind slab that stepped down to the November facets.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">There was also a small wind slab (size 1.0) that was naturally triggered in the past 24hrs on a steep wind affected East aspect at 2300m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There were a few recent reports of wind slabs to size 2 occurring on north and east-facing terrain at treeline and above. The wind slabs formed in response to strong southwest winds and snowfall on Thursday and Friday. Continued snowfall and strong westerly winds on Sunday and Monday morning will likely spark another round of wind slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">A Windslab has been reported size 2.0 that was about 20 cm deep and ran 300 metres. Explosives control released a couple of 50 cm deep pockets in the alpine size 2.5</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday, natural and skier triggered wet sluffing was reported from steep sun exposed slopes. Similar activity is still possible on Monday. Human-triggering of old wind slabs also remains possible in isolated areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Forecast sunny skies may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There was surprisingly little reported avalanche activity given the amount of new snow and wind on Thursday and Friday. Size 1 soft slabs were reportedly sensitive to human triggering in high elevation lee terrain. Looking forward, more wind and snow on Sunday and Monday will likely spark a round of natural storm slab activity. New new snow will also add more stress to these recently buried weaknesses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported. Forecast new snow and wind are expected to increase the size and frequency of windslab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Forecast sunny skies may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several windslab avalanches up to size 2.0 were reported on Sunday that were 20-30 cm deep on northerly aspects in the alpine and at treeline. I suspect that the size and likelihood of windslab and new storm snow avalanches has increased with the new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Several reports of windslabs up to size 1.5 on various aspects in the alpine that were 20-30 cm deep. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently. It may still be possible to trigger old pockets of wind slabs or loose snow sluffs from steep sun-exposed slopes, especially if conditions remain warm and sunny.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, a skier-triggered slab released on a weak layer near the ground in Kananaskis Country. Otherwise there has been no new avalanche activity reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday a skier triggered a size 2.0 full depth slide on a steep and shallow south aspect at 2700m. No injuries or burial, but the skier was carried approximately 400m down slope. The last 48 hours have seen an increase in wind slab activity as well. These have all been small, thin wind slabs triggered either naturally or by skiers in the alpine and open areas at treeline. Typically the trigger zones are steep and unsupported features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There were a few recent reports of wind slabs to size 2 occurring on north and east-facing terrain at treeline and above. In addition, local skiers are reporting&nbsp; activity on solar aspects.&nbsp; With incoming storms, more wind slab development&nbsp; ( and avalanches )&nbsp; can be expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Several cornice falls up to size 2.5 were reported on Monday. Continued strong westerly winds are developing windslabs on lee aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported recently. Loose wet slides or cornice falls remain possible with the continued mild and sunny weather. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Forecast sunny skies may increase the likelihood of loose wet avalanches on solar aspects, as well as cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There has been little avalanche activity reported given the amount of new snow and wind on Thursday and Friday last week. Size 1 soft slabs were reported to be sensitive to human triggering in high elevation lee terrain. Things should stabilize slowly given the warm temperatures, but incoming storms later in the week will likely spark another round of natural storm slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Several windslab avalanches were reported from Sunday up to size 2.0 that were 20-50 cm deep on northerly aspects in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday, there was a report of a size 2 natural wind slab avalanche from a southeast aspect at around 1400 m. There was also a report of a small (size 1) skier-triggered wind slab from a west facing slope. This slide averaged 30 cm din depth. Another observer noted that the recent 10 cm of snow was not bonding well to the previous crust and was sliding easily on any steep slope. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Forecast sunny skies may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Poor visibility due to rain and fog limited travel on Monday. I suspect that new storm slabs developed in the alpine, and rain may have resulted in loose wet releases below 2000 metres.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">One report of a skier triggered windslab size 1.5 on a northeast aspect in the alpine. One report of a large natural icefall size 2.5 that did not release a slab from the slope below</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported in the past several days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, a skier-triggered slab released on a weak layer near the ground in Kananaskis Country. Otherwise there has been no new avalanche activity reported from the region. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2.5 slab avalanche occurred in the past 24 to 48 hours on a steep south-west aspect at 2700m on Snow Peak. The avalanche was a wind slab, but it is suspected to have been triggered by solar radiation in the shallow snowpack start zone. Several loose wet avalanches up to size 2.0 have also occurred on steep south, south-west and west aspects in the past 2 days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There have been recent reports of skier accidental and natural wind slabs to size 1.5 occurring on north and east-facing terrain at treeline and above. On Tuesday we received a report of a size 2 skier triggered avalanche on Hudsons Bay Mtn. with skier involvement and injuries.&nbsp; Local skiers have also reported natural activity on solar aspects. With incoming storms, more wind slab development ( and avalanches ) can be expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported for a few days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Forecast sunny skies may increase the likelihood of loose wet avalanches on solar aspects, as well as cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There has been little avalanche activity reported given the amount of new snow from the last storm. Size 1 skier triggered wind slabs have been reported in high elevation lee terrain. Incoming precipitation will change things up and may spark another round of natural storm slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">A couple of skier controlled pockets of windslab up to size 1.0 were reported from Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A few wet snow avalanches have been reported occurring on solar aspects. Cloudy skies may keep the surface from overnight freezing and increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, remotely skier-triggered avalanches up to size 2 were reported from as far as 40m away. These were releasing on the mid-February weak crust/facet layer and typically occurred in wind loaded areas. </span><span class="s_3FE45715">On Thursday, light rain at lower elevations may further destabilize the warm upper snowpack and loose wet avalanches should be expected. Up high where the new precipitation falls as snow, wind slab formation is expected to continue. Finally, with the combination of unseasonably warm temperatures with little overnight recovery, recent strong solar inputs, and forecast rain, there is a concern for dormant persistent weak layers to wake-up which could result in large slab avalanches. This is a low probability, high consequence problem but deserves attention as we can expect several more days of warm conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday, natural and skier triggered wet sluffing was reported up to size 2. A natural size 2 was reported to have released on the ground on a SE aspect between 1500-2000m. On Monday, a skier triggered a size 1.5 wind slab on a NE aspect in the alpine.</span><span class="s_3FE45715"> On Thursday, light rain at lower elevations may further destabilize the warm upper snowpack and loose wet avalanches should be expected. Up high where the new precipitation falls as snow, wind slab formation may occur. Finally, with the combination of unseasonably warm temperatures with little overnight recovery, recent strong solar inputs, and forecast rain, there is a concern for dormant persistent weak layers to wake-up which could result in large slab avalanches. This is a low probability, high consequence problem but deserves attention as we can expect several more days of warm conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Apart from small loose wet sluffs triggered by skiers on steep sunny slopes, no new avalanches have been reported in the past several days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, our field team members in the north Elk Valley experienced several whumpfs on south facing treed terrain at 2200 m. They also experienced a whumpf of a hard slab near ridge top at 2450 m and saw a deep slab release on a sunny aspect that probably occurred some time in the last week. Recent loose wet avalanches up to size 1.5 appeared to have been triggered by solar warming. On Sunday, a skier-triggered slab released on a weak layer near the ground in Kananaskis Country. As temperatures remain very warm for the next few days, it might be time to change your thinking and treat the snowpack with more caution than recent conditions have warranted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated loose wet avalanches were noted from steep solar aspects in the afternoon.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">One report from yesterday of a size 2.5 natural that occurred on an East aspect around 2000m. As well, we received a report of a size 2 skier triggered avalanche on Hudsons Bay Mtn. with skier involvement and injuries. Local skiers have also reported natural activity on solar aspects. Both of these avalanches were wind slabs on old surfaces.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Reports from Tuesday of loose wet avalanches and cornice failures from steep sun exposed slopes. No slab avalanches have been reported recently in the Purcells but there were some concerning avalanches in the Columbia regions. An natural avalanche failed near the ground in the South Columbia region and multiple skier-triggered avalanches were reported in the North Columbia region. On Thursday, light rain at lower elevations may further destabilize the warm upper snowpack and loose wet avalanches should be expected. Up high where the new precipitation falls as snow, wind slab formation is expected to continue. Finally, with the combination of unseasonably warm temperatures with little overnight recovery, recent strong solar inputs, and forecast rain, there is a concern for dormant persistent weak layers to wake-up which could result in large slab avalanches. This is a low probability, high consequence problem but deserves attention as we can expect several more days of warm conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only small loose wet avalanches have been reported over the last few days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported. Forecast sunny skies may increase the likelihood of loose wet avalanches on solar aspects, as well as cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There has been little avalanche activity reported given the amount of new snow from the last storm. Size 1 skier triggered wind slabs have been reported in high elevation lee terrain. Incoming precipitation will change things up and may spark another round of natural storm slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday, a large skier triggered avalanche resulted in a fatality (See: http://www.cbc.ca/news/canada/british-columbia/avalanche-kills-backcountry-ski-guide-near-golden-b-c-1.2990448). Several other skier triggered avalanches were also reported including remotely triggered avalanches. This includes wind slabs and persistent slabs over the mid-February weak layer. </span><span class="s_3FE45715">On Thursday, light rain at lower elevations may further destabilize the warm upper snowpack and loose wet avalanches should be expected. Up high where the new precipitation falls as snow, wind slab formation is expected to continue. Finally, with the combination of unseasonably warm temperatures with little overnight recovery, recent strong solar inputs, and forecast rain, there is a concern for dormant persistent weak layers to wake-up which could result in large slab avalanches. This is a low probability, high consequence problem but deserves attention as we can expect several more days of warm conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A few wet snow avalanches have been reported occurring on solar aspects. Cloudy skies may keep the surface from overnight freezing and&nbsp; rising teemperatures may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, several natural size 2 avalanches were reported but no details were provided.&nbsp; A skier remote avalanche was also reported to have been triggered from 20m away. Finally, ski cuts released several small pockets of wind slab which were overlying the crust/facet layer. On Tuesday, remotely skier-triggered avalanches up to size 2 were reported from as far as 40m away. These were releasing on the mid-February weak crust/facet layer and typically occurred in wind loaded areas. </span><span class="s_3FE45715">On Friday, sunny and warm conditions are expected to destabilize the snowpack again. Large avalanches have isolated potential to release on deep weak layers. Sluffing is expected from steep sun-exposed slopes and the triggering of wind slabs is possible in the alpine.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday and Wednesday, several natural avalanches were reported to have released on the ground. These were on solar aspects and the largest was a size 3. Natural and skier triggered wet sluffing was also reported up to size 2. </span><span class="s_3FE45715">On Friday, sunny and warm conditions could produce similar conditions. Large avalanches have isolated potential to release on deep weak layers or the ground. Sluffing is expected from steep sun-exposed slopes and the triggering of wind slabs is possible in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Apart from small loose wet sluffs triggered by skiers on steep sunny slopes, no new avalanches have been reported in the past several days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, our field team members in the north Elk Valley experienced several whumpfs on south facing treed terrain at 2200 m. They also experienced a whumpf of a hard slab near ridge top at 2450 m and saw a deep slab release on a sunny aspect that probably occurred some time in the last week. Recent loose wet avalanches up to size 1.5 appeared to have been triggered by solar warming. On Sunday, a skier-triggered slab released on a weak layer near the ground in Kananaskis Country. As temperatures remain very warm for the next few days, it might be time for a mentality shift. Treat the snowpack with more caution than in recent weeks. Large avalanches are becoming more likely again.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated loose dry avalanches noted on steep south</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">No reports of avalanche activity from yesterday, but that is probably because of poor weather and lack of observations.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Thursday, a natural cornice failure triggered a wind slab on the slope below. On Tuesday, loose wet avalanches and cornice failures from steep sun exposed slopes were reported. There have been some concerning avalanches in the neighboring Columbia regions including natural slabs releasing to ground and reactive wind slabs over facets being remotely triggered.&nbsp; </span><span class="s_3FE45715">On Friday, sunny and warm conditions are expected to destabilize the snowpack. Large avalanches have isolated potential to release on deep weak layers. Sluffing is expected from steep sun-exposed slopes and the triggering of wind slabs is possible in the alpine.</span><span class="s_17AE1194" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only small loose wet avalanches have been reported over the last few days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">No new avalanches have been reported.Forecast sunny skies may increase the likelihood of loose wet avalanches on solar aspects, and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There was no avalanche activity reported in the region yesterday, but this may be a case of poor weather and limited observations.&nbsp; Size 1 skier triggered wind slabs have been previously reported in high elevation lee terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Wednesday, a size 1.5 skier triggered persistent slab was reported at the north of the region.&nbsp; This released on the mid-Feb layer down 40cm on a small convex feature. On Tuesday, a large skier triggered avalanche resulted in a fatality (See: http://www.cbc.ca/news/canada/british-columbia/avalanche-kills-backcountry-ski-guide-near-golden-b-c-1.2990448). Several other skier triggered avalanches were also reported including remotely triggered avalanches. This includes wind slabs and persistent slabs over the mid-February weak layer.&nbsp; In the South Columbia region, several avalanches released to ground on solar aspect slopes.&nbsp; </span><span class="s_3FE45715">On Friday, sunny and warm conditions are expected to destabilize the snowpack. Large avalanches have isolated potential to release on deep weak layers. Sluffing is expected from steep sun-exposed slopes and the triggering of wind slabs is possible in the alpine.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">One report from yesterday of a natural wind slab avalanche, size 2, on a North East aspect, wind-loaded at 2000m.  A few wet snow avalanches have been reported occurring on solar aspects. Cloudy skies may keep the surface from overnight freezing and rising temperatures may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, natural, skier-triggered, and explosive-triggered avalanches were reported up to size 2.5. Much of this activity is releasing on the mid-February layer down 30-60cm. On Wednesday, several natural size 2 avalanches were reported but no details were provided. A skier remote avalanche was also reported to have been triggered from 20m away. Finally, ski cuts released several small pockets of wind slab which were overlying the crust/facet layer. </span><span class="s_3FE45715">Saturday's storm is expected to quickly build touchy new wind slabs where the precipitation falls as snow. At lower elevations where the precipitation falls as rain, loose wet avalanches can be expected. The major question and my biggest concern is whether deeply buried persistent weaknesses will wake-up with the new loading. These persistent weak layers could have the potential to result in some very large persistent slab avalanches. However, this is probably a low probability, high consequence type of problem.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday through Thursday, several natural avalanches were reported to have released on the ground. These were on solar aspects and the largest were size 3. Natural and skier triggered wet sluffing was also reported up to size 2. On Thursday, several small wind slabs were triggered by skiers.  Saturday's storm is expected to quickly build touchy new wind slabs where the precipitation falls as snow.  At lower elevations where the precipitation falls as rain, loose wet avalanches can be expected.  </span><span class="s_3FE45715">The major question and my biggest concern is whether deeply buried persistent weaknesses will wake-up with the new loading. These persistent weak layers could have the potential to result in some very large persistent slab avalanches. However, this is probably a low probability, high consequence type of problem.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Apart from small loose wet sluffs triggered by skiers on steep sunny slopes, no new avalanches have been reported in the past several days. Rain, snow and strong winds are expected to drive some avalanche activity this weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, our field team members in the north Elk Valley experienced several whumpfs on south facing treed terrain at 2200 m. They also experienced a whumpf of a hard slab near ridge top at 2450 m and saw a deep slab release on a sunny aspect that probably occurred some time in the last week. Recent loose wet avalanches up to size 1.5 appeared to have been triggered by solar warming. On Sunday, a skier-triggered slab released on a weak layer near the ground in Kananaskis Country. Rain, snow and wind forecast for the weekend are likely to drive natural avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No activity today</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Commercial operators closer to the coast are reporting up to 50cm of new snow in the past 24hrs with rain up to treeline and above.&nbsp; Limited observations due to low cloud from this storm.&nbsp; No avalanches observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Thursday, a cornice failure triggered a small wind slab on the slope below and a natural size 2 slab was reported from a steep rocky sun-exposed slope.&nbsp; There have been some concerning avalanches in the neighboring Columbia regions over the last few days including natural slabs releasing to ground and very reactive wind slabs over facets being remotely triggered. </span><span class="s_3FE45715">Saturday's storm is expected to quickly build touchy new wind slabs where the precipitation falls as snow.  At lower elevations where the precipitation falls as rain, loose wet avalanches can be expected.  The major question and my biggest concern is whether deeply buried persistent weaknesses will wake-up with the new loading.  These persistent weak layers could have the potential to result in some very large persistent slab avalanches.  However, this is probably a low probability, high consequence type of problem.</span><span class="s_17AE1194" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only small loose wet avalanches have been reported over the last few days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Numerous explosive triggered avalanches to size 1.5 reported yesterday as well as one 1.5 skier accidental&nbsp; on a wind slab. Forecast sunny skies may increase the likelihood of loose wet avalanches on solar aspects, and with recent warm temperatures, cornice failures should be on the &quot;lookout list&quot;.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Explosive control by a commercial operator yesterday produced numerous size 1.5 to 2 avalanches in the recent storm slab 23 to 35cm thick. In the Ningunsaw, several size 2 moist avalanches were observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Thursday, natural and skier triggered slab avalanches up to size 2 were reported.  These were mainly wind slabs in the alpine.  On Wednesday, a size 1.5 skier triggered persistent slab was reported at the north of the region. This released on the mid-Feb layer down 40cm on a small convex feature. In the South Columbia region, several avalanches released to the ground on solar aspect slopes during the last few days. </span><span class="s_3FE45715">Saturday's storm is expected to quickly build touchy new wind slabs where the precipitation falls as snow. At lower elevations where the precipitation falls as rain, loose wet avalanches can be expected. The major question and my biggest concern is whether deeply buried persistent weaknesses will wake-up with the new loading. These persistent weak layers could have the potential to result in some very large persistent slab avalanches. However, this is probably a low probability, high consequence type of problem.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">On Friday, a snowmobiler accidentally triggered a size 1 wind slab at treeline on a NE aspect. Naturally-triggered loose avalanches were also observed. During the week several small (size 1-1.5) wind slabs were observed on open lee and cross-loaded features throughout the region. A natural avalanche cycle is anticipated to occur in response to snow, wind and rising temperatures on Friday and Saturday. Wind slabs may linger beyond the end of the storm.</span><span class="s_71516F31" /></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A few natural slabs have been reported that are supected to have occurred in the past 24 hrs, most likely during the height of the recent wind, snow, and warm temperature event. Also a natural size 2 initiated by a cornice failure , 20 to 30cm thick, and running on an old sruct.  A few wet snow avalanches have been reported occurring on solar aspects. Cloudy skies may keep the surface from overnight freezing and rising temperatures may increase the likelihood of loose wet avalanches and cornice failures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Friday, widespread natural activity up to size 3 was reported in parts of the region. This was in response to very warm temperatures and strong sun. These avalanches were mainly in the alpine and were reported on all aspects. However, the largest avalanches were reported from north aspects. Much of this activity was releasing on the mid-February layer down 30-60cm. On Sunday, touchy wind slabs are expected in the alpine and it may still be possible to trigger wet sluffing at lower elevations. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Friday, reported activity was limited to loose wet avalanches from steep sun-exposed slopes. On Tuesday through Thursday, several natural avalanches were reported to have released on the ground. These were on solar aspects and the largest were size 3. Natural and skier triggered wet sluffing was also reported up to size 2. On Thursday, several small wind slabs were triggered by skiers. </span><span class="s_3FE45715">On Sunday, touchy wind slabs are expected in the alpine and loose wet sluffing is possible from steep slopes at lower elevations.  There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches.</span><span class="s_17AE1194" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. I suspect wet conditions with poor visibility have limited observations. Heavy precipitation in the south of the region may have resulted in loose wet and wet slab avalanches in areas that have not had a re-freeze for several days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. On Tuesday, our field team members in the north Elk Valley experienced several whumpfs on south facing treed terrain at 2200 m. They also experienced a whumpf of a hard slab near ridge top at 2450 m and saw a deep slab release on a sunny aspect that probably occurred some time in the last week. Recent loose wet avalanches up to size 1.5 appeared to have been triggered by solar warming. On Sunday, a skier-triggered slab released on a weak layer near the ground in Kananaskis Country. Rain, snow and wind forecast for the weekend are likely to drive natural avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Only a few loose wet slides were observed on Saturday.  Conditions were obscured for most of the day. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Limited observations yesterday because of the intensity and low ceilings associated with the storm. One commercial operation, however,  produced impressive results with explosives and reported several size 1.5's,  2 size 2's, and one size 3 avalanche in the recent storm slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Friday, numerous loose wet avalanches up to size 2 were reported from solar aspect slopes. On Thursday, a cornice failure triggered a small wind slab on the slope below and a natural size 2 slab was reported from a steep rocky sun-exposed slope. During the last few days there have been some concerning avalanches in the neighboring Columbia regions including natural slabs releasing to ground and very reactive wind slabs over facets being remotely triggered. On Sunday, touchy wind slabs are expected in the alpine and loose wet sluffing is possible from steep slopes at lower elevations. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. I suspect that rain up to ridge tops has increased the likelihood of loose wet avalanches. Several days without a re-freeze combined with rain may result in wet slab avalanches. New windslabs are expected to develop in the alpine and at treeline during the next wave of precipitation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Reports from yesterday tell of a few size 1 storm slab, wind slab and  loose-wet avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Limited observations yesterday because of the intensity and low ceilings associated with the storm. One commercial operation, however,  produced impressive results with explosives and reported several size 1.5's,  2 size 2's, and one size 3 avalanche in the recent storm slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Friday, lots of natural loose wet avalanches up to size 2 were reported. Several small slab avalanches were reported to have been triggered by sluffs. A skier triggered a size 2 wind slab on an east aspect in the alpine which was 10-30cm thick. On Thursday, natural and skier triggered slab avalanches up to size 2 were reported. These were mainly wind slabs in the alpine. </span><span class="s_3FE45715">On Sunday, touchy wind slabs are expected in the alpine and it may still be possible to trigger wet sluffing at lower elevations. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">1 size 2 storm slab observed on a NW aspect in steep alpine terrain. Limited observations from yesterday due to low ceilings and poor visibility.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No observations were reported on Saturday due to the storm conditions. </span><span class="s_AA239A9B">On Friday, widespread natural activity up to size 3 was reported in parts of the region. This was in response to very warm temperatures and strong sun. These avalanches were mainly in the alpine and were reported on all aspects. However, the largest avalanches were reported from north aspects. Much of this activity was releasing on the mid-February layer down 30-60cm. </span><span class="s_3FE45715">On Monday, touchy storm slabs are expected in the alpine and possibly at treeline. There is some uncertainty regarding the distribution of these storm slabs but they could be widespread. Thicker winds slabs associated with the storm are expected in leeward features and are the biggest concern for Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Observations were limited on Saturday due to the storm conditions but explosive and skier-triggered avalanches up to size 1.5 were reported from all aspects and above 1900m.&nbsp; </span><span class="s_3FE45715">On Monday, touchy storm slabs are expected in the alpine and possibly at treeline.&nbsp; There is some uncertainty regarding the distribution of these storm slabs but they could be widespread.&nbsp; Thicker winds slabs associated with the storm are expected in leeward features and are the biggest concern for Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. I expect new snow and wind to create fresh windslabs that may be very touchy to human triggers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. I expect that forecast new snow and wind will develop new storm slabs in the alpine and at treeline on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing was observed or reported today, but observations were very limited due to poor visibility. It is expected that a natural avalanche cycle will begin late Sunday or early Monday in the alpine and at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">There are numerous reports of large avalanches up to size 4 from yesterday.  Commercial operators and Min. of Highways have reported evidence of a large natural cycle that  occurred during or towards the end of this last storm..</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations were limited on Saturday due to the storm conditions but ski cuts produced size 1 slab avalanches. On Monday, touchy storm slabs are expected in the alpine and possibly at treeline, especially in the south of the region. There is some uncertainty regarding the distribution of these storm slabs but they could be widespread. Thicker winds slabs associated with the storm are expected in leeward features and are the biggest concern for Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. I expect that new storm slabs are developing on all aspects in the alpine and at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Reports from yesterday tell of a few size 1 storm slabs, wind slab and loose-wet avalanches. Explosive testing has produced few results</span></p>
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</style><p class="p_CC664AAA"><span class="s_A9A7295C">Reports from late yesterday tell of numerous large, size 2 and 3,&nbsp; natural and explosive controlled storm slab avalanches above 1000m as well as loose-wet natural avalanches between 1000 to 1500m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations were limited on Saturday due to the storm conditions but natural and explosive-triggered storm slab avalanches up to size 2 were reported. On Monday, touchy storm slabs are expected in the alpine and possibly at treeline. There is some uncertainty regarding the distribution of these storm slabs but they could be widespread. Thicker winds slabs associated with the storm are expected in leeward features and are the biggest concern for Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Touchy wind slabs have formed on lee and cross-loaded slopes following southerly winds. These can be triggered by the weight of a person, even from a distance.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, reports of numerous size 1-3 natural slab avalanches and skier remote avalanches were observed. Many of these larger events started as wind and storm slab avalanches from upper elevation start zones and entrained moist snow at lower elevations, running to valley bottoms. These avalanches have occurred on a variety of aspects with northerly aspects being most reactive. These have initiated from 2000-2300 m in elevation. Most of these failures have been on a weak storm shear. I suspect that the deeper releases are occurring on the mid-February layer down 30-70cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, reports of numerous size 1-3 natural slab avalanches and skier remote avalanches have been observed. Many of these larger events started as wind and storm slab avalanches from upper elevations. These avalanches have occurred on a variety of aspects with northerly aspects being most reactive. These have initiated from 2000-2800 m in elevation. With forecast sunshine and solar radiation, touchy slab avalanches are expected in the alpine and loose wet sluffing is possible from steep solar slopes at all elevations. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At the time of publishing this bulletin no new avalanche activity had been reported. My best guess is that there was a healthy round of storm slab activity in response to all the new snow and wind on Sunday. Looking forward, I`m sure the new storm slab will remain sensitive to human triggering in high elevation, wind-exposed terrain. Also, sun on Tuesday will likely spark a round of loose wet/ wet slab avalanche activity on steeper, sun-exposed slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At the time of publishing this bulletin no new avalanche activity had been reported. My best guess is that there was a healthy round of storm slab activity in response to all the new snow and wind on Sunday. Looking forward, I`m sure the new storm slab will remain sensitive to human triggering in high elevation, wind-exposed terrain. Also, sun on Tuesday will likely spark a round of loose wet/ wet slab avalanche activity on steeper, sun-exposed slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several naturally triggered loose avalanches (both dry and wet) occurred on all aspects in steep terrain at alpine and treeline elevations up to size 1.5. In addition, ski cutting produces sluffs up to size 1.5 on steep north facing terrain. A few slab avalanches also occurred in the past 24hrs. These are all naturally triggered slabs (some by solar triggering) and occurred in alpine terrain on all aspects up to size 2.0.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A large and widespread natural avalanche cycle occurred last week and into Saturday. On Sunday, skiers triggered several size 1 storm slabs on steep lee features. </span><span class="s_AA239A9B">Click on the blue dot on the map to see a recent wind slab that may have failed naturally or remotely in Sinclair. It was a thick, hard wind slab on a north aspect. There are likely to more like this lurking. </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Natural loose wet avalanche activity has been reported on N-NW aspects from 2100-2700 m. Explosive controlled slab avalanches up to size 3 were also reported from northerly aspects above 2400 m. During the last few days there have been some concerning avalanches in the neighboring Columbia regions including natural slabs releasing to ground and very reactive wind slabs over facets being remotely triggered. On Tuesday, touchy slab avalanches are expected in the alpine and loose wet sluffing is possible from steep slopes at all elevations due to the effects of solar radiation. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches, especially in shallower snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">At the time of publishing this bulletin no new avalanche activity had been reported. My best guess is that there was a healthy round of storm slab activity in response to all the new snow and wind on Sunday. Looking forward, I`m sure the new storm slab will remain sensitive to human triggering in high elevation, wind-exposed terrain. Also, sun on Tuesday will likely spark a round of loose wet/ wet slab avalanche activity on steeper, sun-exposed slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">A cycle of wind slabs (most size 1, up to size 2) was reported on Sunday. These failed naturally and were triggered remotely by skiers as well. Many were on north aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Explosives control on Sunday triggered several very large avalanches near Stewart, failing at ground or on a deeply buried crust. Last week there was a widespread natural avalanche cycle. No naturally triggered avalanches were reported on Sunday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, reports of numerous size 1-3.5 natural slab avalanches and skier remote avalanches have been observed. Many of these larger events started as wind and storm slab avalanches from upper elevation start zones and entrained moist snow at lower elevations, running to valley bottoms. These avalanches have occurred on a variety of aspects with northerly aspects being most reactive. These have initiated from 2000-2300 m in elevation. Most of these failures have been on a weak storm shear. I suspect that the deeper releases are occurring on the mid-February layer down 30-80 cm. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">Throughout last weekend, numerous wind slabs to size 2 were reported. Although the recently formed wind slabs may be gaining strength in some areas, I would expect ongoing human triggering in steeper, unsupported terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A cycle of wind slabs and storm slabs (most size 1, up to size 2) was reported on Sunday and Monday. These failed naturally and were triggered remotely by skiers as well. Many were on north aspects.</span><span class="s_3D0464D1"> A snowmobiler also triggered an avalanche on Sunday (see http://bit.ly/19wEv36).</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, the region saw natural slab avalanches up to size 2.5, and numerous remotely triggered avalanches size 1-2.5 from 500 m away. All of the remotely triggered avalanches failed on the mid-February crust buried 30-60 cm below the surface non north-east aspects above 2000 m. This type of fracture character and remote triggering is very unpredictable. A conservative approach and terrain use is required with these conditions. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, reports of numerous size 1-2.5 natural slab avalanches and skier triggered avalanches have been observed. These avalanches have occurred on a variety of aspects with northerly aspects being most reactive. These have initiated from 2000-2600 m in elevation. A couple of these slab avalanches were triggered remotely from 50 m away an there is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday, a natural size 2 avalanche was reported from a steep wind-loaded slope, ski cuts produced several size 1 soft storm slabs, and a skier triggered a size 1.5 storm slab. Lots of natural loose wet avalanches up to size 2 were reported from all aspects in the afternoon. On Wednesday, loose wet avalanches are possible during the heat of the afternoon, especially on sun-exposed slopes. Human-triggering of storm slabs remains a major concern, especially in the alpine. Wind-loaded features and steep, unsupported slopes are the most likely areas to trigger an avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We haven't received any reports recently but this likely speaks to a lack of observers. In the Lizard region, </span><span class="s_3FE45715">a natural avalanche cycle up to size 2.5 was reported with slabs up to 80cm thick. Similar activity is expected to have occurred in the South Rockies Region. On Wednesday, human-triggering of storm slabs remains a major concern, especially in the alpine. Wind-loaded features and steep, unsupported slopes are the most likely areas to trigger an avalanche. Loose wet avalanches are possible during the heat of the afternoon, especially on sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several solar triggered sluffs up to size 2.0 observed today in the alpine. A few slab avalanches up to size 2.0 were also observed in steep alpine terrain on all aspects. These slabs involved only the storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday, a skier triggered a size 2 wind slab on a NE aspect at 1300 m. Several loose avalanches also failed on steep sunny slopes. On Sunday, skiers triggered several size 1 storm slabs on steep lee features. Click on the blue dot on the map to see a recent wind slab that may have failed naturally or remotely in Sinclair. It was a thick, hard wind slab on a north aspect. There are likely to more like this lurking.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday, several natural slab avalanches up to size 2.5 were reported. Most of these initiated from northerly aspects 2000-2500 m in elevation. Numerous explosive controlled slab avalanches were also initiated up to size 2.There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger persistent slab avalanches, especially in shallower snowpack areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday, a natural avalanche cycle up to size 2.5 was reported. These were storm slabs up to 80cm thick. Loose sluffing was also reported from steep terrain at all elevations. </span><span class="s_3FE45715">On Wednesday, human-triggering of storm slabs remains a major concern, especially in the alpine. Wind-loaded features and steep, unsupported slopes are the most likely areas to trigger an avalanche. Loose wet avalanches are possible during the heat of the afternoon, especially on sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A skier accidentally triggered a size 3 hard wind slab on Monday, which failed on the March crust/facet layer. Skiers also remotely triggered size 1.5-2.5 slabs, most on northerly aspects, some of which failed on the crust/facet layer. A natural and human-triggered cycle of wind slabs was reported on Sunday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Monday, several loose avalanches to size 1.5 were observed on solar aspects. A skier triggered a size 1 wind slab in the alpine. </span><span class="s_71516F31">Explosives control on Sunday triggered several very large avalanches near Stewart, failing at ground or on a deeply buried crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, reports of numerous size 1-2.5 natural slab avalanches and natural cornice failures were reported. Several rider triggered and remotely triggered wind slab and storm slab avalanches were seen from a variety of aspects and 1900-2600 m in elevation. Most of these failures continue to be on a weak storm shear interface. Deeper releases are occurring on the persistent mid-February layer down 30-60 cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A cycle of wind slabs and storm slabs (mostly size 1, up to size 2) was reported on Sunday and Monday. These failed naturally and were triggered remotely by skiers as well. Many were on north aspects.</span><span class="s_3D0464D1"> A snowmobiler also triggered an avalanche on Sunday in the Hurley area (check out the blue pin on our forecast map). On Wednesday, a size 2 slab avalanche was remotely triggered from a distance of 100m. The avalanche failed on a north aspect at 2050m between the Duffey Lake road and Gates Lake. This avalanche failed on the recently buried crust/facet combo, and speaks to the potentially touchy nature of the interface. New snow and wind on Thursday will likely spark a new new round of wind slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, reports from the region indicated numerous natural slab avalanches up to size 2.5, and a skier remote (15 m away) slab avalanche size 2, failing on the mid-February facet/ crust interface which remains alive and well.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, numerous natural slab avalanches and skier triggered avalanches up to size 2 were reported. Most of these avalanches failed on northerly aspects above 2000 m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Tuesday, natural loose wet avalanches to size 2 were reported. Skier-triggered avalanches up to size 1.5 were also reported. These occurred on all aspects and elevations, and were reported to have released on the mid-March crust. On Monday, a natural size 2 avalanche was reported from a steep wind-loaded slope, ski cuts produced several size 1 soft storm slabs, and a skier triggered a size 1.5 storm slab. Lots of natural loose wet avalanches up to size 2 were reported from all aspects on Monday afternoon. On Thursday, loose wet avalanches are possible during afternoon, especially if the rain starts early. Human-triggering of wind slabs in the alpine remains the main concern. This problem is probably isolated to high elevation north aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle to size 2.5 occurred on Monday during the storm. These were primarily storm slab avalanches but several stepped down to deeper persistent weak layers or to the ground in steep unskiable terrain. At lower elevations, loose wet avalanches up to size 2.5 were reported as well as isolated wet slabs. Natural activity quickly tapered off following the storm but the storm slab is expected to still be reactive to human-triggering. It is best to avoid steep unsupported slopes and convexities, as well as steep gully features. There is also concern for avalanches to step down to deeper persistent weak layers in isolated areas. Loose wet avalanches are a concern on sun-exposed slopes during the heat of the afternoon. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanche activity was observed.  But field teams were out of the area by early afternoon. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday, a skier triggered a size 2 wind slab on a NE aspect at 1300 m. Several loose avalanches also failed on steep sunny slopes. Click on the blue dot on the map to see a recent wind slab that may have failed naturally or remotely in Sinclair. It was a thick, hard wind slab on a north aspect. There are likely to more like this lurking. New snow and wind on Thursday will likely promote further wind slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday, several natural slab avalanches up to size 2 were reported from northerly-easterly aspects above 1800 m.  Numerous explosive controlled slab avalanches were also initiated up to size 1.5 on easterly aspects above 2300 m. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger slab avalanches, especially in shallower snowpack areas.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle to size 3 occurred on Monday during the storm. These were primarily storm slab avalanches up to 80cm thick. At lower elevations, loose wet avalanches up to size 2.5 were also reported. On Tuesday, explosives triggered several storm slabs up to size 2.5. On Thursday, the storm slab is expected to still be reactive to human-triggering. It is best to avoid steep unsupported slopes and convexities, as well as steep gully features. Loose wet avalanches are a concern on sun-exposed slopes during the heat of the afternoon.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A skier accidentally triggered a size 3 hard wind slab on Monday, which failed on the March crust/facet layer. Skiers also remotely triggered size 1.5-2.5 slabs, most on northerly aspects, some of which failed on the crust/facet layer. A natural and human-triggered cycle of wind slabs was reported on Sunday. A round of storm slab activity is expected over the next few days in response to forecast snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555"> A skier recently triggered a size 1 wind slab in the alpine. Explosives control on Sunday triggered several very large avalanches near Stewart, failing at ground or on a deeply buried crust. New snow and wind on Wednesday night and Thursday is expected to promote a new round of storm slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, reports of natural avalanche activity seemed to taper off; however, numerous human triggered and explosive triggered slab avalanches were reported up to size 2 mostly on northerly aspects above 2100 m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">On Wednesday, a size 2 slab avalanche was remotely triggered from a distance of 100 m. The avalanche failed on a north aspect at 2050 m between the Duffey Lake road and Gates Lake. This avalanche failed on the recently buried crust/facet combo, and speaks to the potentially touchy nature of the interface. Skiers also remotely triggered a size 2, which sympathetically triggered a size 1 slab, on the same persistent weak layer on a north aspect. New snow and wind may overload this weakness, creating destructive avalanches. A cycle of wind slabs and storm slabs (mostly size 1, up to size 2) was reported on Sunday and Monday. These failed naturally and were triggered remotely by skiers as well. Many were on north aspects. A snowmobiler also triggered an avalanche on Sunday in the Hurley area (check out the blue pin on our forecast map).</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, natural and skier triggered slab avalanches were reported up to size 2. Both avalanches were reportedly over steeper convex terrain features on northerly aspects above 2100 m. Widespread natural avalanche activity is expected through the weekend due to new snow, rain and strong SW winds. Avalanches failing on the the mid-February persistent interface will likely have wide propagations and be large and destructive. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, several natural slab avalanches and skier triggered avalanches up to size 2 were reported. Most of these avalanches failed on north- easterly aspects above 2000 m. With forecast snow, rain and wind, widespread natural avalanche activity is expected through the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Wednesday, loose wet activity was reported from steep rocky sun-exposed slopes. Skiers were also triggering wet sluffs during the heat of the day. On Tuesday, natural loose wet avalanches to size 2 were reported. Skier-triggered avalanches up to size 1.5 were also reported. These occurred on all aspects and elevations, and were reported to have released on the mid-March crust. On Friday, loose wet avalanches are possible during the heat of the day, especially if there is rain or periods of sun. In the alpine, old wind slabs may still be reactive and new wind slabs are expected to be building with the current strong SW winds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle to size 2.5 occurred on Monday during the storm. These were primarily storm slab avalanches but several stepped down to deeper persistent weak layers or to the ground in steep unskiable terrain. At lower elevations, loose wet avalanches up to size 2.5 were reported as well as isolated wet slabs. </span><span class="s_3FE45715">On Friday, wind loaded areas are the biggest concern.  New wind slabs will be touchy and may overload older wind slabs in leeward terrain features. Loose wet avalanches are a concern on sun-exposed slopes during the heat of the afternoon or areas that receive rain.</span><span class="s_AA239A9B" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations from today. There were numerous loose wet avalanches from yesterday's heat. All aspects/elevations had loose wet issues. The largest would have been sz2.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">On Monday, a skier triggered a size 2 wind slab on a NE aspect at 1300 m. Several loose avalanches also failed on steep sunny slopes. Click on the blue dot on the map to see a recent wind slab that may have failed naturally or remotely in Sinclair. It was a thick, hard wind slab on a north aspect. There are likely to more like this lurking. More snow and wind will likely promote further wind slab activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Wednesday, a couple of natural slab avalanches up to size 2 were reported from northerly and westerly aspects above 2300 m.&nbsp; Explosive controlled slab avalanches up to size 2 were also initiated in steeper terrain features on north-easterly aspects. There is a still a concern for avalanches to step down to deeply buried weak layers resulting in larger slab avalanches, especially in shallower snowpack areas. With new snow, rain and strong winds natural avalanche activity will likely persist through the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle to size 3 occurred on Monday during the storm. These were primarily storm slab avalanches up to 80cm thick. At lower elevations, loose wet avalanches up to size 2.5 were also reported. On Tuesday and Wednesday, explosives triggered storm slabs up to size 2.5. On Wednesday, a natural size 2 loose wet avalanche was reported from a NE aspect slope and a skier trigger a size 1.5 loose wet avalanche. On Friday, wind loaded areas are the biggest concern.  New wind slabs will be touchy and may overload older wind slabs in leeward terrain features. Loose wet avalanches are a concern on sun-exposed slopes during the heat of the afternoon or areas that receive rain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">A size 2.5 avalanche was observed from a distance on a north aspect at 2300 m. It is suspected to have been remotely triggered by a snowmobiler. A skier accidentally triggered a size 3 hard wind slab on Monday, which failed on the March crust/facet layer. Skiers also remotely triggered size 1.5-2.5 slabs, most on northerly aspects, some of which failed on the March crust/facet layer. A natural and human-triggered cycle of wind slabs was reported on Sunday. A round of storm slab activity is expected over the next few days in response to forecast snow and wind. Because of the buried persistent weak layer, avalanches might be bigger than expected for the amount of new snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555"> Explosives triggered a size 1.5 wind slab on Wednesday. A skier also recently triggered a size 1 wind slab in the alpine. Explosives control on Sunday triggered several very large avalanches near Stewart, failing at ground or on a deeply buried crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, natural slab avalanches and cornice failures were reported up to size 2, with one cornice failure slab size 3. Most of these occurred on north-easterly aspects above 1900 m. Smaller skier triggered avalanches were also reported up to size 1.5. With steady rain, snow and windy conditions, natural large avalanches are likely to continue through the weekend. Avalanches failing on the buried persistent layers will likely be large and destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Over the past week, isolated slab avalanches to size 2 have occurred on persistent weaknesses buried on March 11th. In a few cases, avalanches failed with light inputs such as remote triggers. New snow and wind will create its own mix of reactive surface instabilities, but it will also add load to these deeper, more destructive layers. There's a fair bit of uncertainty as to how the March 11th interface will react to storm loading. That said, I'd resist heading into aggressive higher elevation as any releases on this layer would likely be destructive in nature.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Thursday was a fairly stormy day and observations are minimal but I suspect natural avalanche activity occurred. On Wednesday, natural and skier triggered slab avalanches were reported up to size 2. Both avalanches were reportedly over steeper convex terrain features on northerly aspects above 2100 m. Widespread natural avalanche activity is expected through the weekend with new snow, rain and strong SW winds. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, numerous size 1-2 storm slabs and loose dry avalanches up to 1.5 were reported. Wednesday, several natural slab avalanches and skier triggered avalanches up to size 2 were reported. Most of these avalanches failed on north- easterly aspects above 2000 m. With forecast snow, rain and wind, natural avalanche activity is expected to continue tomorrow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, skiers were triggering wet sluffing and natural dry sluffing was reported on steep north facing features. On Wednesday, natural and skier-triggered sluffing was reported from steep sun-exposed slopes. </span><span class="s_3FE45715">On Saturday, wind loaded areas are the biggest concern. New wind slabs will likely be touchy. Loose wet avalanches are a problem at lower elevations where it is raining. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A widespread natural avalanche cycle to size 2.5 occurred on Monday during the storm. These were primarily storm slab avalanches but several stepped down to deeper persistent weak layers or to the ground in steep unskiable terrain. At lower elevations, loose wet avalanches up to size 2.5 were reported as well as isolated wet slabs. Natural avalanches quickly tapered off during the storm but touchy conditions existed through the week. Winds increased on Thursday and wind slab formation has been ongoing since. With strong winds and precipitation continuing on Saturday, </span><span class="s_3FE45715">wind slabs will continue to build and are expected to be touchy. Loose wet avalanches are a problem at lower elevations where it is raining. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations from today. </span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">I'm sure human wind slab triggering will be possible over the weekend. Check out the blue dot on our Forecast Region Overview Map for details on a recently triggered wind slab avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Thursday a skier controlled size 1.0 slab avalanche was reported. However, the snow and wind didn't start up in the Purcell region until Thursday afternoon. I suspect some natural avalanche activity occurred on Friday. A concern still exists for avalanches to step down to deeply buried weak layers, especially in shallower snowpack areas. With new snow, rain and strong winds natural avalanche activity will likely continue through the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle to size 3 occurred on Monday during the storm. These were primarily storm slab avalanches up to 80cm thick. At lower elevations, loose wet avalanches up to size 2.5 were also reported. On Tuesday and Wednesday, explosives triggered storm slabs up to size 2.5. On Wednesday, a natural size 2 loose wet avalanche was reported from a NE aspect slope and a skier trigger a size 1.5 loose wet avalanche. No new avalanches were reported on Thursday. On Saturday, wind loaded areas are the biggest concern. New wind slabs will be touchy. Loose wet avalanches are a problem at lower elevations where it is raining. </span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Over the past week, isolated slab avalanches to size 2.5 have occurred on persistent weaknesses buried on March 11th. In a few cases, avalanches failed with light inputs such as remote triggers. New snow and wind will create its own mix of reactive surface instabilities, but it will also add load to these deeper, more destructive layers. There's a fair bit of uncertainty as to how the March 11th interface will react to storm loading. That said, I'd resist heading into aggressive higher elevation as any releases on this layer would be destructive in nature.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, explosives control triggered wind slab avalanches to size 1.5.</span></p><p class="p_CC664AAA"><span class="s_1681A555">No other recent avalanches were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, numerous storm slab avalanches up to size 2 were reported. Wednesday saw natural slab avalanches and cornice failures up to size 2, with one cornice failure slab size 3. Most of these occurred on north-easterly aspects above 1900 m. With steady rain, snow and windy conditions, natural large avalanches are likely to continue tomorrow. Avalanches failing on the buried persistent layers. will likely be large and destructive</span></p>
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</style><p class="p_CC664AAA"><span class="s_C6F15715">Wind slab avalanches to size 2 have been observed in the last week. On Wednesday, our field team observed a size 2 wind slab avalanche from a NW facing feature at about 1400m. On Saturday, touchy new wind slabs are expected to be widespread in leeward terrain features. These wind slabs may remain reactive for a few days after the wind dies down on Sunday. Persistent avalanches are not expected to be a problem but isolated avalanches could step down to a deeper layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Over the past week, isolated slab avalanches to size 2 have occurred on persistent weaknesses buried on March 11th. In a few cases, avalanches failed with light inputs such as remote triggers from distances of up to 100m away. New snow and wind has created its own mix of reactive surface instabilities, but it has also added load to these deeper, more destructive layers. There's a fair bit of uncertainty as to how the March 11th interface will react to storm loading. That said, I'd resist heading into aggressive higher elevation as any avalanches on this layer would likely be destructive in nature.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanches observations have been limited due to the storm conditions but a widespread natural avalanche cycle is expected to be occurring at higher elevations. On Friday, several natural size 2 avalanches were observed. On Wednesday, natural and skier triggered slab avalanches were reported up to size 2. On Sunday, natural activity is expected to taper off as temperatures become cooler. However, if the sun is out in the afternoon, natural avalanches are possible from sun-exposed slopes. Human-triggering of storm slabs is expected to be a major concern for the next few days, especially at higher elevations where the snow is still dry.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday and Friday, numerous storm slabs up to size 2 were reported. This were primarily human-triggered and typically above 2000m. Numerous natural loose wet avalanches up to 1.5 were also reported from lower elevations. With the additional loading on Saturday, natural storm slab avalanches are expected to be occurring. On Sunday, natural activity is expected to taper off as temperatures become cooler. However, if the sun is out in the afternoon, natural avalanches are possible from sun-exposed slopes. Human-triggering of storm slabs is expected to be a major concern for the next few days, especially at higher elevations where the snow is still dry.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous natural and rider triggered avalanches to size 2 were reported Friday as moist storm snow slid on the robust mid-March crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity to report from Friday. A widespread natural avalanche cycle to size 2.5 occurred on Monday during the storm. These were primarily storm slab avalanches but several stepped down to deeper persistent weak layers or to the ground in steep unskiable terrain. At lower elevations, loose wet avalanches up to size 2.5 were reported as well as isolated wet slabs. Natural avalanches quickly tapered off during the storm but touchy conditions existed through the week. Winds increased on Thursday and wind slab formation has been ongoing since. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new was observed today, but observation were limited.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Wind slab triggering may be possible over the weekend. Loose wet avalanche to size 2 were also observed in steep, below treeline terrain. Forecast sunny breaks may promote ongoing loose wet avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Thursday, a natural size 2 wind slab was reported from an east aspect at 2400m. A skier controlled size 1 wind slab avalanche was reported from an east aspect at 2600m. No new slab avalanches were observed on Friday but loose sluffing from steep terrain features was reported. On Sunday, thin wind slabs are expected to reactive to human-triggering.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose moist avalanches to size 1.5 ran on all aspects as high as 2100m on Friday. After Mondays storm a widespread natural avalanche cycle ran to size 3. These were primarily storm slab avalanches up to 80cm thick. At lower elevations, loose wet avalanches up to size 2.5 were also reported. On Tuesday and Wednesday, explosives triggered storm slabs up to size 2.5. On Wednesday, a natural size 2 loose wet avalanche was reported from a NE aspect slope and a skier trigger a size 1.5 loose wet avalanche. </span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Over the past week, isolated slab avalanches to size 2.5 have occurred on persistent weaknesses buried on March 11th. In a few cases, avalanches failed with light inputs such as remote triggers. New snow and wind has promoted widespread storm slab avalanche activity, but it has also added load to these deeper, more destructive layers. There's a fair bit of uncertainty as to how the March 11th interface will react to storm loading. That said, I'd resist heading into aggressive higher elevation as any releases on this layer would be destructive in nature.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, explosives control triggered wind slab avalanches to size 2 in the north of the region.</span></p><p class="p_CC664AAA"><span class="s_1681A555">No other recent avalanches were reported. With sunny breaks forecast for the next few days loose wet avalanches are possible in sun-exposed terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday and Friday, numerous storm slab avalanches up to size 2 were reported. This includes both natural and human-triggered avalanches. At many elevations the storm slabs were moist or wet and were running on a crust layer. Lots of loose wet avalanches have also been observed recently. On Sunday, natural activity is expected to taper off as temperatures become cooler overnight. However, if the sun is out in the afternoon, natural avalanches are possible from sun-exposed slopes. Human-triggering of storm slabs is expected to be a major concern for the next few days, especially at higher elevations where the snow is still dry. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Over the past week, there have been a number of avalanches to size 2.5 occurring on the March 11 persistent weak layer. Some avalanches have occurred naturally, or remotely from distances of up to 100m. Hot spots for avalanche activity seem to include the Duffey Lake area, the Birkenhead drainage, the Hurley and the South Chilcotins. Snow and wind on Monday will likely add a round of wind slab activity to the mix. But it will also add load to the March layer, potentially adding to its reactivity and destructive potential. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle occurred on Saturday with storm slabs up to size 3 being reported. These avalanches were failing on a crust layer from mid-March and also stepping down to a deeper crust/facet layer from mid-February. At lower elevations, these slabs were moist or wet. In the N Columbia region, many remotely triggered avalanches were reported from up to 100m away. Unfortunately, a fatality occurred in the Cariboo region from a very large avalanche that released on the mid-February layer. This layer is expected to remain touchy for longer than normal and human-triggered avalanches remain a major concern for Monday, especially for steep alpine features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle occurred on Saturday with storm slabs up to size 3 being reported. These avalanches were failing on a crust layer from mid-March or within the storm snow. At lower elevations, these slabs were moist or wet. Human-triggered avalanches remain a major concern for Monday, especially for steep alpine features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Saturday there were reports of a few loose wet slides up to size 1.5. Numerous natural and rider triggered avalanches to size 2 were reported Friday as moist storm snow slid on the robust mid-March crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There are no reports of new avalanches for the past couple days. Neighbouring regions reports minimal loose wet sluffing from steep terrain on Saturday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few loose wet up to size 1.0 on steep terrain on all aspects below treeline as well as on solar aspects up to mountain top.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Numerous size 1 loose wet avalanches were reported on Saturday. They failed in steep rocky terrain in response to warming and solar radiation. Cloud on Monday should limit this type of pattern, although there may be a shift to small wind slab activity with light convective snowfall forecast for Monday morning.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Saturday in the deeper snowfall areas, natural storm slab avalanches were reported. Explosives triggered avalanches up to size 2.5 which were up to 100cm deep. In the Dogtooth, touchy wind slabs were reported. On Monday, thin wind slabs are expected to reactive to human-triggering. Where enough new snow exists, it may be possible to trigger storm slab avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose wet avalanches to size 1.5 were observed on all aspects between 1600 and 2000m on Friday and Saturday. Isolated wind slabs and cornice falls remain possible, especially as the sun comes ou and temperatures rise.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Over the past week, isolated slab avalanches to size 2.5 have occurred on persistent weaknesses buried on March 11th. In a few cases, avalanches failed with light inputs such as remote triggers. Recent heavy snowfall and wind prior to the weekend resulted in widespread storm slab avalanche activity to size 2, but it has also added load to these deeper, more destructive layers.  On Sunday, numerous large slab avalanches were observed in the Spearhead Range and on Ipsoot Mtn. The March 11 interface was the suspected culprit in most of these events.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, a few isolated size 1 wind slabs were skier triggered in the north of the region. No other avalanches were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle occurred on Saturday with storm slabs up to size 3 being reported.  These avalanches were failing on a crust layer from mid-March and also stepping down to a deeper crust/facet layer from mid-February.  At lower elevations, these slabs were moist or wet.&nbsp; Many remotely triggered avalanches were reported from up to 100m away.  Unfortunately, a fatality occurred in the Cariboo region from a very large avalanche that released on the mid-February layer.  This layer is expected to remain touchy for longer than normal and human-triggered avalanches remain a major concern for Monday, especially for steep alpine features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, there have been a number of avalanches to size 2.5 occurring on the March 11 persistent weak layer. Some avalanches have occurred naturally, or remotely from distances of up to 100m. Hot spots for avalanche activity seem to include the Duffey Lake area, the Birkenhead drainage, the Hurley and the South Chilcotins. Snow and wind on Monday night will likely add a round of wind slab activity to the mix. But it will also add load to the March layer, potentially adding to its reactivity and destructive potential. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle occurred on Saturday with storm slabs up to size 3 being reported. On Sunday, natural avalanches tapered off but were still occurring on sun-exposed slopes. Many explosive and human-triggered storm slab avalanches were reported on Sunday. These avalanches were failing on a crust layer from mid-March and also stepping down to a deeper crust/facet layer from mid-February.  At lower elevations, these slabs were moist or wet. Many remotely triggered avalanches were reported from up to 100m away. On Tuesday, human-triggered storm slabs and persistent slabs remain a serious concern, especially in steep alpine terrain. If an avalanche steps down to the persistent weak layer, very large and destructive avalanches are possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle occurred on Saturday with storm slabs up to size 3 being reported. These avalanches were typically failing 40-60cm deep but were over 1m deep in wind loaded areas. At lower elevations, these slabs were moist or wet. On Sunday, natural avalanches tapered off but were still occurring on sun-exposed slopes. Many explosive and human-triggered storm slab avalanches were also reported on Sunday. There were several remotely triggered avalanches with the farthest being triggered from 100m away. One cornice triggered slab avalanche is expected to have stepped down to a deep weak layer from January. On Tuesday, human-triggered storm slab avalanches remain a concern, especially in steep alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Sunday several size 1-2 storm slabs were reported from the northern part of the region. These were all from NW-NE aspects between around 2000 and 2300 m. One slide was reported as a size 2.5 that may have been triggered by a cornice fall and may have released on the mid March crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There are no new reports of avalanches for the past couple days. However, there is potential for touchy storm or wind slabs at and above treeline and loose wet slides below treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed today.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous size 1 loose wet avalanches were reported on Saturday. They failed in steep rocky terrain in response to warming and solar radiation.  On Sunday cornice failures to size 2 were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Saturday in the deeper snowfall areas, a natural avalanche cycle to size 2.5 was reported. These were storm slabs were typically 40-60cm thick but were up to 1m deep in wind loaded areas. On Sunday, explosives triggered numerous more storm slab avalanches. On a glacier feature, one of these explosive triggered avalanches stepped down 250cm to the glacial ice. Human-triggered avalanches were also reported including a remotely triggered avalanche from 35m away. In the Dogtooth, touchy size 1 wind slabs were being skier triggered and explosives produced a size 2 with slab depth of 20-50cm. On Tuesday, human-triggered storm slabs remain a concern for the deeper snowfall areas while wind slabs are a concern for the rest of the region. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several natural and skier controlled loose wet avalanches to size 1.5 were observed on all aspects between 1600 and 2000m on Sunday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, isolated slab avalanches to size 2.5 have been running on the mid-March persistent weak layer. In a few cases, avalanches failed with light inputs such as remote triggers. Recent heavy snowfall and wind prior to the weekend resulted in widespread storm slab avalanche activity to size 2, but it has also added load to these deeper, more destructive layers. On Sunday, numerous large slab avalanches were observed in the Spearhead Range and on Ipsoot Mtn. The mid-March interface was the suspected culprit in most of these events. See this observation for a good visual: http://bit.ly/1CS2Nld http://bit.ly/1CS2Nld </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, a few isolated size 1 wind slabs were skier triggered in the north of the region.  On Sunday cornice fall to size 2 was observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A widespread natural avalanche cycle occurred on Saturday with storm slabs up to size 3 being reported. On Sunday, natural avalanches tapered off but were still occurring on sun-exposed slopes. Many explosive and human-triggered storm slab avalanches were reported on Sunday. These avalanches were failing on a crust layer from mid-March and also stepping down to a deeper crust/facet layer from mid-February. At lower elevations, the slab avalanches were moist or wet. Many remotely triggered avalanches were reported from up to 100m away. On Tuesday, human-triggered storm slabs and persistent slabs remain a series concern, especially in steep alpine terrain. If an avalanche steps down to the persistent weak layer, very large and destructive avalanches are possible. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, there have been a number of avalanches to size 2.5 occurring on the March 11 persistent weak layer. Some avalanches have occurred naturally, or remotely from distances of up to 100m. Hot spots for avalanche activity seem to include the Duffey Lake area, the Birkenhead drainage, the Hurley and the South Chilcotins.  No new activity to report from Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, the region continued to see numerous natural slab avalanches up to size 2.5 from all aspects and 2000-2500 m in elevation. These avalanches were failing on a crust layer from mid-March and also stepping down to a deeper crust/facet layer from mid-February. Human-triggered storm slabs and persistent slabs remain a serious concern, especially in steep alpine terrain. Remote triggering slab avalanches from afar also remain a concern. If an avalanche does step down to the persistent weak layer, very large and destructive avalanches are possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday afternoon we received a report of a human triggered persistent slab avalanche size 2.5 on a northerly aspect at 2000 m. On Monday, numerous natural and human triggered slab avalanches were reported up to size 2.5 with the majority failing in the recent storm snow and the deeper mid-March interface. There were several remotely triggered avalanches with the farthest being triggered from 150 m away. On Wednesday, I suspect natural avalanche activity to taper off; however, remote human triggering remains a major concern up to size 2.5. Avalanches that fail on the deeper weak interfaces will be large and destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Sunday and Monday a few size 1-2 storm slabs were reported from the northern part of the region. These were all from NW-NE aspects between around 2000 and 2300 m. One slide on Sunday was reported as a size 2.5 that may have been triggered by a cornice fall and appeared to release on the mid March crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There are no new reports of avalanches from the region for the past couple days. However, widespread natural slab avalanche to size 1.5 above 1800 m were reported from the Fernie area on Monday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new was observed or reported today.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous size 1 loose wet avalanches were reported on Saturday. They failed in steep rocky terrain in response to warming and solar radiation. On Sunday cornice failures to size 2 were reported. Several small wind slabs from immediately lee of ridge crest were reported Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday, several natural avalanches up to size 2 on north and west aspects were reported. Explosive control showed avalanches up to size 2 mostly from northerly aspects above 2300 m. On Wednesday, wind slabs are expected to reactive to human-triggering. Where enough new snow exists, it may be possible to trigger storm slab avalanches up to size 2.5.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread natural slab avalanches up to size 1.5 were reported above 1800 m on Monday. On Sunday, most of the reported activity was small loose wet slides between 1600 and 1900 m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, very large slab avalanches have been running to size 3, failing on the mid-March persistent weak layer.  This interface remains very reactive, avalanches have been remote triggered by skiers as recently as Monday.  See this observation for a good visual: http://bit.ly/1CS2Nld </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, a few isolated size 1 wind slabs were skier triggered in the north of the region. On Sunday cornice fall to size 2 was observed. No new avalanche activity to report from Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, numerous natural and human triggered slab avalanches were reported up to size 2.5 with the majority failing in the recent storm snow and down deeper on the mid-March interface. The persistent mid-February interface remains a layer of concern and is primed for human triggering. This layer is expected to remain touchy for longer than normal and human-triggered avalanches remain a major concern, especially for steep alpine features.&nbsp; Unfortunately this region saw fatalities last weekend. For technical details regarding this incident go here: http://old.avalanche.ca/cac/library/incident-report-database/view/12b2631a-5b7f-4f0e-a2d8-c6f89bfb494d</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, there have been a number of avalanches to size 2.5 occurring on the mid-March persistent weak layer. Some avalanches have occurred naturally and many have been remote triggered from up to 100m away. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, the region continued to see numerous natural slab avalanches up to size 2.5 from all aspects and 2000-2500 m in elevation. Natural cornice failures up to size 2 were also reported from southeast aspects near 2600 m. Some of avalanches were failing on a crust layer from mid-March and also stepping down to a deeper crust/facet layer from mid-February. Human-triggered storm slabs and persistent slabs remain a serious concern, especially in steep alpine terrain. Remote triggering slab avalanches from afar also remain a concern. There is currently a Special Avalanche Warning for this region through the forecast period. For more technical information regarding the fatalities last weekend go here: old.avalanche.ca/cac/library/incident-report-database/view/12b2631a-5b7f-4f0e-a2d8-c6f89bfb494d</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Tuesday, numerous natural solar induced slab avalanches were reported, with the majority being size 1. We also received numerous reports of human triggered slab avalanches up to size 2, mostly running on N-NE aspects and above 2000 m. Explosive controlled avalanches were also initiated up to size 3. Most of these avalanches from Tuesday failed within the recent storm interface and on the mid-March persistent interface. With a warm, wet and windy storm in the forecast natural and human triggered avalanche activity will likely continue. Avalanches that fail on the deeper weak interfaces will be large and destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported on Tuesday. On Sunday and Monday a few size 1-2 storm slabs were reported from the northern part of the region. These were all from NW-NE aspects between around 2000 and 2300 m. One slide on Sunday was reported as a size 2.5 that may have been triggered by a cornice fall and appeared to release on the mid March crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There are no new reports of avalanches from the region for the past couple days. However, neighbouring regions reported some loose dry slides on Tuesday and widespread natural slab avalanches to size 1.5 above 1800 m on Monday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new natural avalanche activity was noted. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small wind slab avalanches were reported from alpine features Tuesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday we received two separate reports of a skier triggered storm slab size 2 and a remotely triggered slab size 3 which occurred on Monday. A solar induced natural avalanche cycle occurred tuesday afternoon up to size 2, and explosive controlled size 2-3 slab avalanches were initiated from steep N-NE aspects above 2300 m. On Thursday, wind slabs are expected to be touchy and reactive to human-triggering. Where enough new snow exists, it may be possible to trigger storm slab avalanches up to size 3.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few small loose dry avalanches were reported from steep alpine/treeline terrain on Tuesday. Widespread natural slab avalanches up to size 1.5 were reported above 1800 m on Monday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, very large slab avalanches have been running to size 3, failing on the mid-March persistent weak layer. What makes this spooky is that the majority of these avalanches have been remote triggered, some from as far as 200m away. This interface remains very reactive. While it's a few days old now, the photo in this Mountain Information Network post provides a very powerful visual: http://bit.ly/1CS2Nld </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Observed avalanche activity from Tuesday was limited to one small skier triggered storm slab on a NE facing feature around 2000m in the southern portion of the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, numerous natural and human triggered slab avalanches were reported up to size 3.5 with the majority failing in the recent storm snow and down deeper on the mid-February interface. This persistent layer of concern is also responsible for a couple of remotely triggered (110 m away) slab avalanches up to size 2.5 which were initiated from a north and a west aspect above 1700 m. This layer is expected to remain touchy for longer than normal and human-triggered avalanches remain a major concern, especially for steep alpine features. There is currently a Special Avalanche Warning for this region through the forecast period. For more technical information regarding the fatalities last weekend go here: old.avalanche.ca/cac/library/incident-report-database/view/12b2631a-5b7f-4f0e-a2d8-c6f89bfb494d</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, there have been a number of avalanches to size 2.5 occurring on the mid-March persistent weak layer. Some avalanches have occurred naturally and many have been remote triggered from up to 100m away. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, no new avalanches were reported. Earlier in the week, widespread natural and human triggered avalanches were reported up to size 2.5. With forecast warm, wet and windy weather widespread natural avalanche activity is likely. Human-triggered storm slabs and persistent slabs remain a serious concern, especially in steep alpine terrain. Remote triggering slab avalanches from afar also remain a concern. There is currently a Special Avalanche Warning for this region through the forecast period. For more technical information regarding the fatalities last weekend go here: old.avalanche.ca/cac/library/incident-report-database/view/12b2631a-5b7f-4f0e-a2d8-c6f89bfb494d.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, several natural large cornice failures up to size 2.5 were reported along with a natural size 2 storm slab from NW-SE aspects above 2200 m. I suspect the region saw a  natural avalanche cycle with Thursday's storm, however; reports across the region have yet confirmed distribution, size and magnitude. On Friday, natural avalanche activity will likely continue with warm temperatures, strong winds and periods of sun and rain. Avalanches failing on the mid-March persistent interface will be large and destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported on Tuesday or Wednesday. On Sunday and Monday a few size 1-2 storm slabs from NW-NE aspects between 2000-2300 m were reported from the northern part of the region. One slide on Sunday was reported as a size 2.5 that may have been triggered by a cornice fall and appeared to release on the mid March crust. Warming a rain moved in by early Thursday which may have resulted in more widespread storm slab and wet activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent observations are limited. The only new reports are of minor loose snow sluffing out of steep terrain in the Fernie area. Light rain and warming temperatures early on Thursday could kick off a more widespread loose wet or wet slab cycle. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited observations today. Its suspected that there was an isolated loose wet cycle late this afternoon at treeline and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small wind slab avalanches were reported from alpine features Tuesday. Reports from Wednesday include numerous wet loose avalanches reaching Size 2 on steep rocky slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were reported on Wednesday, but visibility was poor. On Monday a size 3 was remotely triggered from a steep unsupported roll, and a size 2 was accidentally triggered by skiers. Both occurred on N-NE aspects around 2200-2300m and were 20 to 50cm deep. A solar induced natural avalanche cycle occurred Tuesday afternoon up to size 2 on southerly aspects, and explosive controlled size 2-3 slab avalanches were initiated from steep N-NE aspects above 2300 m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Recent observations are limited. The only new reports are of minor loose snow sluffing out of steep terrain. Light rain and warming temperatures early on Thursday could kick off a more widespread loose wet or wet slab cycle. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, very large slab avalanches have been running on the mid-March persistent weak layer. What makes this spooky is that the majority of these avalanches have been remote triggered, some from as far as 200m away. This interface remains very reactive. While it's a few days old now, the photo in this Mountain Information Network post provides a very powerful visual: http://bit.ly/1CS2Nld </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches were reported on Wednesday, but poor weather hampered observations. On Tuesday a skier triggered a small storm slab on a NE facing feature around 2000m in the southern portion of the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, large natural wet slab avalanches up to size 3 slab were reported. Loose wet activity also occurred up to size 1.5 out of steep terrain features at treeline and below. On Wednesday, no natural avalanche activity was reported, however; numerous explosive triggered slabs up to size 1.5 were initiated from N-NW slopes above 2000 m. Skier triggered avalanches were also reported up to size 1.5 on wind loaded N-E aspects. With forecast warm, wet and windy weather natural avalanche activity will likely continue. Human-triggered storm slabs and persistent slabs remain a serious concern, especially in steep alpine terrain. Remote triggering slab avalanches from afar also indicate the sensitivity of the persistent weak layer. There is currently a Special Avalanche Warning for this region through the forecast period. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, there have been a number of avalanches to size 2.5 occurring on the mid-March persistent weak layer. Some avalanches have occurred naturally and many have been remote triggered from up to 100m away. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">In the Cariboo region no new avalanches were reported on Thursday, however; in the North Columbia Mountains south of the Cariboo's, warm, wet and windy weather was responsible for a widespread natural avalanche cycle up to size 3. With similar weather conditions, I'd hedge my bets that this was also the story in the Cariboo's. I suspect natural avalanche activity will likely continue with warm temperatures, strong winds and periods of sun and rain. Avalanches failing on the persistent interface will be large and destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Warm, wet and windy weather on Thursday was responsible for a widespread natural avalanche cycle which occurred on all aspects above 1900 m up to size 2.5. Numerous human triggered slab avalanches up to size 1.5 and loose wet avalanches up to size 1.5 were also reported. I suspect natural avalanche activity will likely continue with warm temperatures, strong winds and periods of sun and rain. Avalanches failing on the mid-March persistent interface will be large and destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm slabs ran to size 2 on all aspects Thursday as cold snow was subjected to rapidly warming temperatures. Loose wet avalanches ran on all aspects to size 2.5. The larger loose avalanches were running on north through west facing terrain between 1900m and 2100m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent observations. In the neighboring Lizard Range Thursday was filled with natural loose wet activity to size 1.5 between 1700m and 2100m on N/NE faces. One natural size 2 wet slab was also recorded on an unknown aspect. On Friday our field team reported continued widespread loose wet avalanches and wet slabs to size 2 that were entraining significant mass as they moved downhill. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet avalanches were observed on solar aspects and at lower elevations up to sz 1. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include continued natural wet loose avalanche activity up to Size 2 on steep rocky slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Thursday, wind and warming conditions were responsible for several natural slab avalanches up to size 3 from east and north aspects above 2100 m. There was also a report of a close call, skier triggered size 2.5 slab avalanche from the Dogtooth range. Extensive snowballing, and small loose wet avalanches were also reported from slopes below 2200 m. If some areas of the region see convective snow/ rain (20 mm) overnight Friday, and strong westerly winds, natural avalanche activity will likely continue on Saturday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Thursday was filled with natural loose wet activity to size 1.5 between 1700m and 2100m on N/NE faces. One natural size 2 wet slab was also recorded on an unknown aspect. On Friday our field team reported continued widespread loose wet avalanches and wet slabs to size 2 that were entraining significant mass as they moved downhill. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, very large slab avalanches have been running on the mid-March persistent weak layer. What makes this spooky is that the majority of these avalanches have been remote triggered, some from as far as 200m away. This interface remains very reactive. While it's a few days old now, the photo in this Mountain Information Network post provides a very powerful visual: http://bit.ly/1CS2Nld </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several natural storm slab avalanches up to Size 3 were reported on Thursday. Many of them occurred on Wednesday. Storm and wind slabs were also highly reactive to human triggers on Thursday with several skier-controlled avalanches up to Size 1.5 running on a buried crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Warm, wet and windy weather on Thursday was responsible for a widespread natural avalanche cycle which occurred on all aspects up to size 3. Numerous human triggered slab avalanches up to size 1.5 and loose wet avalanches up to size 1.5 were also reported. I suspect natural avalanche activity will likely continue with warm temperatures, strong winds and periods of sun and rain. Avalanches failing on either of the two persistent weak interfaces will be large and destructive. There is currently a Special Avalanche Warning for this region through the forecast period. </span></p>
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</style><p class="p_CC664AAA"><span class="s_C6F15715">Throughout the past week, numerous loose wet avalanches were reported failing on steeper, sun-exposed slopes. No other avalanches were reported. There may be a transition to new wind slab activity with new snow and wind forecast for Saturday night.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, there have been a number of avalanches to size 2.5 occurring on the mid-March persistent weak layer. Some avalanches have occurred naturally and many have been remote triggered from up to 100m away. </span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">A natural avalanche cycle to size 2.5 was observed on Friday. These were slabs 60-100 cm deep on north aspects, and loose wet avalanches on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">A widespread avalanche cycle ran on Thursday and Friday in response to wet and windy conditions. These were a mix of storm slab, loose wet avalanches and persistent slabs, up to size 3. A few remotely triggered avalanches were also reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A wide variety of avalanches were observed Friday: Loose wet avalanches to size 2 on all aspects between 1600m and 2200m, a size 2 wet slab on a E/SE facing feature at 2200m and even a rider triggered storm slab on an E facing feature, likely from early in the day.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent observations. In the neighboring Lizard Range numerous loose wet avalanches and a few wet slabs were observed to size 2 on Friday. Our field team also reported continued widespread loose wet avalanches and wet slabs to size 2 that were entraining significant mass as they moved downhill.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose wet up to size 2.0 observed on all aspects below 2400m. Extensive snowballing at treeline and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche reports.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> </span><span class="s_3D0464D1">On Thursday and Friday, wind and warming were responsible for several natural slab avalanches up to size 3, mainly on east and north aspects above 2100 m. There was also a report of a close call, skier triggered size 2.5 slab avalanche in the Dogtooth range. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose wet avalanches and a few wet slabs were observed to size 2 on Friday. Our field team also reported continued widespread loose wet avalanches and wet slabs to size 2 that were entraining significant mass as they moved downhill. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past week, very large slab avalanches have been running on the mid-March persistent weak layer. What makes this spooky is that the majority of these avalanches have been remote triggered, some from as far as 200m away. This interface remains very reactive. While it's a few days old now, the photo in this Mountain Information Network post provides a very powerful visual: http://bit.ly/1CS2Nld </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, a size 2.5 avalanche was triggered on a north aspect in the alpine. The avalanche appeared to be triggered from relatively low angle terrain and ran in a layer of surface hoar buried around 40 cm below the surface. There were several reports of other deliberately triggered avalanches (ski cuts and explosive triggered avalanches) that could be easily triggered up to size 2. These ran on NW to NE aspects between 1400 and 2100 m. On Thursday, at least four natural avalanches up to size 2.5 were reported from north aspect slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A snowmobiler triggered a size 2.5 slab on Turbo Hill on Boulder Mountain near Revelstoke on Friday. Click on the blue dot on the map for more info. There was also a natural cycle of slabs and loose wet avalanches up to size 3 on Friday. Many of these were persistent slabs failing on the Feb crust and some were loose wet avalanches. Although most of the persistent slab activity was on north aspects, there was some on east and south-east aspects as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, two size 2 wind slab avalanches were reported from the north of the region. For a little over a week, there have been consistent reports of avalanches to size 2.5 occurring on the mid-March persistent weak layer. Some avalanches have occurred naturally and many have been remote triggered from up to 100m away.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">A natural avalanche cycle, size 2-3, was observed on Friday and Saturday. These were slabs up to 100 cm deep and loose wet avalanches on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">On Saturday, a few naturally triggered persistent slabs, size 2-3, were observed. A widespread avalanche cycle ran on Thursday and Friday in response to wet and windy conditions. These were a mix of storm slab, loose wet avalanches and persistent slabs, up to size 3. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity reported from Saturday. A wide variety of avalanches were observed Friday: Loose wet avalanches to size 2 on all aspects between 1600m and 2200m, a size 2 wet slab on a E/SE facing feature at 2200m and even a rider triggered storm slab on an E facing feature, likely from early in the day.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent observations. In the neighboring Lizard Range a size 2.5 avalanche that was likely triggered by cornice fall was observed Saturday, but the bulk of the observed activity was limited to minor sluffing and small loose wet avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche reports.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">On Thursday and Friday, wind and warming were responsible for several natural slab avalanches up to size 3, mainly on east and north aspects above 2100 m. There was also a report of a close call, skier triggered size 2.5 slab avalanche in the Dogtooth range. A couple of small slabs were triggered on Saturday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A size 2.5 avalanche that was likely triggered by cornice fall was observed Saturday, but the bulk of the observed activity was limited to minor sluffing and small loose wet avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We have not yet heard how avalanche activity panned out in response to the recent storms, due to limited visibility and the challenges of backcountry travel at this time. We have previously had ongoing reports of very large slab avalanches running on the mid-March persistent weak layer. I would be very surprised if this layer has not performed during the recent storm cycle.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Information has not yet come in regarding activity from the current storm. On Friday, a size 2.5 avalanche was triggered on a north aspect in the alpine. The avalanche appeared to be triggered from relatively low angle terrain and ran in a layer of surface hoar buried around 40 cm below the surface. There were several reports of other deliberately triggered avalanches (ski cuts and explosive triggered avalanches) that could be easily triggered up to size 2. These ran on NW to NE aspects between 1400 and 2100 m. On Thursday, at least four natural avalanches up to size 2.5 were reported from north aspect slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Saturday, a couple of large naturally-triggered, and one remotely-triggered, slabs were recorded. Loose wet avalanches were also failing where rain or sun was affecting the snow. A snowmobiler was buried in a size 2.5 slab on Turbo Hill on Boulder Mountain near Revelstoke on Friday. Click on the blue dot on the map for more info. There was also a natural cycle of slabs and loose wet avalanches up to size 3 on Friday. Many of these were persistent slabs failing on the Feb crust and some were loose wet avalanches. Although most of the persistent slab activity was on north aspects, there was some on east and south-east aspects as well. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Largely due to inclement weather, recent reports have been fairly scarce. For a little over a week, there have been consistent reports of avalanches to size 2.5 occurring on the mid-March persistent weak layer. Some avalanches have occurred naturally and many have been remote triggered from up to 100m away.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A natural avalanche cycle size 2-3 was reported on Friday and Saturday. These were slabs up to 100 cm deep and loose wet avalanches on all aspects. Observations were limited on Sunday and no new avalanches were reported.  On Monday, several avalanches up to size 3 were reported.  These may have occurred on Sunday or Monday.  One of the size 3 avalanches released down 100cm, most likely on the mid-Feb persistent weak layer.  At below-treeline elevations, avalanches are reported to be scrubbing down to ground.  Natural avalanches are possible on Tuesday as new snow falls at higher elevations and rain falls down low. Human-triggered storm slabs and persistent slabs are a major concern, especially on steep, unsupported slopes. At lower elevations, be cautious of sluffing from steep slopes when it is raining.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Saturday and Sunday, isolated natural size 2-3 persistent slabs were reported. These occurred on a variety of aspects and mainly above 2000m. At lower elevations, lots of loose wet avalanches were reported. On Thursday and Friday, a widespread avalanche cycle occurred in response to wet and windy conditions. These were a mix of storm slab, loose wet avalanches and persistent slabs up to size 3. Natural avalanches are possible on Tuesday as new snow falls at higher elevations and rain falls down low. Human-triggered storm slabs and persistent slabs are a major concern, especially on steep, unsupported slopes. At lower elevations, be cautious of sluffing from steep slopes when it is raining.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity reported from Saturday or Sunday. The last significant round of activity was from Friday which involved wet activity to size 2 on all aspects between 1600m and 2200m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday our field team was in the Crown Mountain area where they noticed a few large slab avalanches on an extreme E/NE face that were likely triggered by cornice fall.&nbsp; On Saturday in the neighboring Lizard Range a size 2.5 avalanche that was likely triggered by cornice fall was observed, but the bulk of the observed activity was limited to minor sluffing and small loose wet avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet cycles continue below treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Storm slabs up to size 2.5 were observed over the weekend in the southwest corner of the region. They formed in response to new snow and wind. No other new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Sunday, several natural avalanches up to size 2 were reported but no details were provided.  These could be new storm slabs or could be failing on deeper layers resulting in persistent slab avalanches. A couple of small skier-triggered soft slabs were triggered on Saturday, most likely from wind loaded features. On Thursday and Friday, wind and warming were responsible for several natural slab avalanches up to size 3, mainly on east and north aspects above 2100 m. There was also a report of a close call, skier triggered size 2.5 slab avalanche in the Dogtooth range.  </span><span class="s_3FE45715">Natural avalanches are possible on Tuesday as new snow falls at higher elevations and rain falls down low. Human-triggered storm slabs and persistent slabs are a concern, especially on steep, unsupported slopes. At lower elevations, be cautious of sluffing from steep slopes when it is raining.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed Sunday. A size 2.5 avalanche that was likely triggered by cornice fall was observed Saturday, but the bulk of the observed activity was limited to minor sluffing and small loose wet avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We have not yet heard how avalanche activity panned out in response to the recent storms, due to limited visibility and the challenges of backcountry travel at this time. We have previously had ongoing reports of very large slab avalanches running on the mid-March persistent weak layer. I would be very surprised if this layer has not performed during the recent storm cycle.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Recent observations have been extremely limited, although I suspect there was a decent round of storm slab activity at higher elevations in response to wet, warm and windy weather over the past few days. On Friday, a size 2.5 avalanche was triggered on a north aspect in the alpine. The avalanche appeared to be triggered from relatively low angle terrain and ran in a layer of surface hoar buried around 40 cm below the surface. There were several reports of other deliberately triggered avalanches (ski cuts and explosive triggered avalanches) that could be easily triggered up to size 2. These ran on NW to NE aspects between 1400 and 2100 m. On Thursday, at least four natural avalanches up to size 2.5 were reported from north aspect slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, a few natural storm slab avalanches were reported. One skier triggered size 1 storm slab in a wind loaded area had a depth of 20-40cm.  On Saturday, a few natural and one remotely-triggered persistent slab avalanches size 2-3.5 were reported. These were releasing on the mid-Feb and mid-March layers down 60-80cm. Loose wet avalanches were also failing where rain or sun was affecting the snow. On Friday during the high elevation rain event, a natural avalanche cycle up to size 3 was reported and included both slabs and loose wet avalanches. Natural avalanches are possible on Tuesday as new snow falls at higher elevations and rain falls down low. Human-triggered storm slabs and persistent slabs are a major concern, especially on steep, unsupported slopes. At lower elevations, be cautious of sluffing from steep slopes when it is raining.</span></p>
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</style><p class="p_CC664AAA"><span class="s_C6F15715">No new avalanche activity to report. Last week numerous loose wet avalanches were reported on steeper, sun-exposed slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, several natural wind slab avalanches to size 2 were observed in the north of the region. In many cases, these wind slabs were triggered by cornice falls. We have not yet heard how persistent avalanche activity panned out in response to the recent storms. My best guess is that we may be transitioning into a lower probability-high consequence avalanche pattern with this persistent weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, several natural size 2-3 avalanches were reported. Details are limited and these may have occurred on Sunday or Monday. One of the size 3 avalanches released down 100cm, most likely on the mid-Feb persistent weak layer. At below-treeline elevations, avalanches are reported to be scrubbing down to ground. A natural avalanche cycle size 2-3 was reported on Friday and Saturday. These were slabs up to 100 cm deep at higher elevations and loose wet avalanches at lower elevations. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural avalanches are generally not expected on Wednesday if there is good overnight recovery but may still be possible in isolated areas. Human-triggered storm slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days and touchy conditions may still exist on Wednesday.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday, a few slab avalanches were reported above around 2200m elevation as well as lots of wet sluffing at lower elevations. Several slabs up to size 2.5 were triggered by cornice failures. Some of these were up to 1m deep and these are expected to be failing on persistent weak layers. On Saturday and Sunday, isolated natural size 2-3 persistent slabs were reported on a variety of aspects and mainly above 2000m. On Thursday and Friday, a widespread avalanche cycle occurred in response to wet and windy conditions. These were a mix of storm slab, loose wet avalanches and persistent slabs up to size 3. </span></p><p class="p_CC664AAA"><span class="s_17AE1194">Natural avalanches are generally not expected on Wednesday if there is good overnight recovery but may still be possible in isolated areas. Human-triggered storm slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days and touchy conditions may still exist on Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday warm temps led to a natural wet slab failure. The size 2 avalanche ran on a steep NE facing feature at 2200m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A few large avalanches were reported on Monday. Our field team was in the Crown Mountain area where they noticed a large slab avalanche on an extreme E/NE face that was likely triggered by cornice fall. In the neighboring Waterton region cornice failure resulted in 2 large avalanches that stepped down to the mid-February interface on NE facing features at 2400m. On Saturday in the neighboring Lizard Range a size 2.5 avalanche that was also likely triggered by cornice fall was observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Two slab avalanches have occurred in the past 48hrs on steep SE aspects in the alpine. These were both size 2.0 and likely triggered by warming and/or solar radiation. In addition, several loose wet avalanches up to size 1.5 were noted on all aspects at treeline and  below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Storm slabs up to size 2.5 were observed over the weekend in the southwest corner of the region. They formed in response to new snow and wind. Touchy wind slabs to size 1.5 were still remotely triggered on Monday. Patterns in avalanche activity vary greatly across the region due to varying recent snowfall amounts and underlying snowpack structure.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Monday, a cornice triggered a size 2 storm slab was reported at 2600m on a NE aspect.  Loose wet sluffing was also reported from lower elevations. On Sunday, several natural avalanches up to size 2 were reported but no details were provided. These could be new storm slabs or could be failing on deeper layers resulting in persistent slab avalanches. A couple of small skier-triggered soft slabs were triggered on Saturday, most likely from wind loaded features. On Thursday and Friday, wind and warming were responsible for several natural slab avalanches up to size 3, mainly on east and north aspects above 2100 m. There was also a report of a close call, skier triggered size 2.5 slab avalanche in the Dogtooth range.  </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Natural avalanches are generally not expected on Wednesday if there is good overnight recovery but may still be possible in isolated areas. Human-triggered wind slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days and touchy conditions may still exist on Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Activity on Monday was limited to small loose wet avalanches. On Saturday a size 2.5 avalanche that was likely triggered by cornice fall was observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, explosives testing produced storm and wind slab avalanches to size 2. These avalanches occurred in response to recent wind and snow. Other than a new size 2.5 persistent slab avalanche on Cowboy Ridge in the Fitzsimmons Range (witnessed on the weekend), we have not yet heard how persistent avalanche avalanche activity panned out in response to the recent storms. My best guess is that we may be transitioning into a lower probability-high consequence avalanche pattern with this persistent layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">In general, observations have been limited in the last few days. That said, in the north of the region several avalanches in the size 1.5-2 range were reported to have been triggered remotely in alpine terrain. The March 25 interface was the culprit in these avalanches. Due to the persistent nature of this interface, avalanche activity on this layer may occur for some time after the stormy weather has ended.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, lots of loose wet avalanches were reported at lower elevations and storm slabs were reported above around 2300m elevation. On Sunday, a few natural storm slab avalanches were reported. One skier triggered size 1 storm slab in a wind loaded area had a depth of 20-40cm. On Saturday, a few natural and one remotely-triggered persistent slab avalanches size 2-3.5 were reported. These were releasing on the mid-Feb and mid-March layers down 60-80cm. On Friday during the high elevation rain event, a natural avalanche cycle up to size 3 was reported and included both slabs and loose wet avalanches. </span></p><p class="p_CC664AAA"><span class="s_17AE1194">Natural avalanches are generally not expected on Wednesday if there is good overnight recovery but may still be possible in isolated areas. Human-triggered storm slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days and touchy conditions may still exist on Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, several natural wind slab avalanches to Size 2 were observed in the north of the region. Two of of the larger avalanches possibly stepped-down to the mid-March persistent weakness on north facing alpine slopes. Also reported were several loose sluffs to Size 1.5 in response to sun-exposure on south aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a natural cornice failure triggered a size 2 slab avalanche with a depth of 40cm.  This occurred on a NE aspect at 2200m elevation.  On Monday, several natural size 2-3 avalanches were reported. Details are limited and these may have occurred on Sunday or Monday. One of the size 3 avalanches released down 100cm, most likely on the mid-Feb persistent weak layer. At below-treeline elevations, avalanches were reported to be scrubbing down to ground. Ongoing persistent slab, storm slab, and loose wet avalanches have been occurring since last Friday. Activity is now expected to taper off with the cooler temperatures. Natural avalanches are generally not expected on Thursday except possibly on steep sun-exposed slopes in the afternoon. Human-triggered storm slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days at higher elevations and tricky conditions may still exist on Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday, two natural size 1.5-2 wind slabs were reported above 2400m elevation. Some natural cornice failures also triggered storm slabs up to size 2. Most of this activity is expected to have occurred in the recent storm snow. On Monday, several natural slab avalanches were reported above around 2200m elevation as well as lots of wet sluffing at lower elevations. Some of these were up to 1m deep and these are expected to be failing on persistent weak layers. Ongoing persistent slab, storm slab, and loose wet avalanches have been occurring since last Friday. Activity is now expected to taper off with the cooler temperatures. Natural avalanches are generally not expected on Thursday except possibly on steep sun-exposed slopes in the afternoon. Human-triggered wind slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days at higher elevations and tricky conditions may still exist on Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity to report from Tuesday. On Monday warm temps led to a natural size 2 wet slab failure that ran on a steep NE facing feature near 2200m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new activity to report from Tuesday. On Monday a few large avalanches were reported: Our field team was in the Crown Mountain area where they noticed a large slab avalanche on an extreme E/NE face that was likely triggered by cornice fall. In the neighboring Waterton region cornice failure resulted in two large avalanches that stepped down to the mid-February interface on NE facing features at 2400m. On Saturday in the neighboring Lizard Range cornice fall produced a size 2.5 avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday include several small natural and skier triggered wind slab avalanches in lee and cross-loaded treeline and alpine terrain. The reports mentioned surprisingly little large avalanche activity given the strong winds and amount of fresh snow available for wind-transport.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">On Tuesday, ski cutting was producing thin wind slabs in the north of the region.&nbsp; On Monday, a cornice triggered a size 2 storm slab was reported at 2600m on a NE aspect. Loose wet sluffing was also reported at lower elevations.&nbsp; </span><span class="s_3FE45715">Ongoing persistent slab, storm slab, and loose wet avalanches have been occurring since last Friday but this activity has tapered off recently. Natural avalanches are generally not expected on Thursday except possibly on steep sun-exposed slopes in the afternoon. Human-triggered wind slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days at higher elevations and tricky conditions may still exist on Thursday.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity to report from Tuesday. Activity on Monday was limited to small loose wet avalanches. On Saturday a size 2.5 avalanche that was likely triggered by cornice fall was observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, explosives testing produced storm and wind slab avalanches and cornice releases to size 2.5. Since the Size 2.5 persistent slab avalanche on Cowboy Ridge in the Fitzsimmons Range on the weekend, we have not received any new reports of persistent avalanche avalanche activity, suggesting that these high consequence avalanches are becoming more stubborn. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Reports from Tuesday include several explosive-controlled wind slab avalanches up to Size 2. In the northern part of the region numerous skier-triggered slabs up to Size 2, including wide propagations and remote triggers, have been associated with a surface hoar weak layer buried on March 25th.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, five natural avalanches size 2-3.5 were reported.  These released down 50-80cm so they likely failed on persistent weak layers.  Wind slabs were reported to be forming in the alpine and loose wet activity was reported at lower elevations. On Monday, lots of loose wet avalanches were reported at lower elevations and storm slabs were reported above around 2300m elevation.  Ongoing persistent slab, storm slab, and loose wet avalanches have been occurring since last Friday. Activity is now expected to taper off with the cooler temperatures. Natural avalanches are generally not expected on Thursday except possibly on steep sun-exposed slopes in the afternoon. Human-triggered storm slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days at higher elevations and tricky conditions may still exist on Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days, several natural cornice falls and wind slab avalanches to Size 2 were observed in the north of the region. Two of of the larger avalanches possibly stepped-down to the mid-March persistent weakness on north facing alpine slopes. Also reported were several loose sluffs to Size 1.5 in response to sun-exposure on south aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, several size 2-3 slabs failed naturally. While the likelihood of triggering a large persistent slab avalanche is decreasing slowly, the consequences remain high.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Persistent slab, storm slab, and loose wet avalanche activity has tapered off recently. While the likelihood of triggering a large avalanche has gone down, the consequences remain high. On Wednesday, a naturally-triggered size 2.5 wind slab was observed on a NE aspect at 2500 m. An ice fall also triggered a size 3 deep persistent slab which failed at ground. Human-triggered wind slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days at higher elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported, although I'm sure there has been some smaller wind slab activity in higher elevation lee terrain in response to recent snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We have had no recent reports of avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday are limited to just one new Size 2 natural wind slab avalanche on a northeast facing alpine slope below a ridge crest. However, reports from Tuesday include several small natural and skier triggered wind slab avalanches in lee and cross-loaded treeline and alpine terrain. The reports mentioned surprisingly little large avalanche activity given the strong winds and amount of fresh snow available for wind-transport.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Ongoing persistent slab, storm slab, and loose wet avalanche activity has tapered off recently. While the likelihood of triggering a large avalanche has gone down, the consequences remain high. On Wednesday, some natural cornice falls were observed on shady aspects, some of which triggered slabs up to size 2.5 on the slopes below. Isolated wind slabs were also reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There have been no new reports of avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday include explosive triggered storm slab avalanches up to Size 2, and one Size 3 persistent slab release on the mid-March persistent weakness.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Reports from Wednesday include several explosive-controlled wind slab avalanches up to Size 2.5 running on facets buried March 25th. A remotely triggered Size 2.5 avalanche released above two skiers catching both of them and burying one, who was successfully recovered. This avalanche failed on the same March 25th weakness, where it was buried surface hoar on a northeast aspect at 1450 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">On Tuesday, five natural avalanches size 2-3.5 were reported. These released down 50-80cm and are suspected to have failed on persistent weak layers. On Wednesday, explosives triggered size 2.5 slabs on lee and cross-loaded slopes. A few cornice falls were also observed.</span></p><p class="p_CC664AAA"><span class="s_3D0464D1">Human-triggered wind slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days at higher elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reported Thursday were several size 2 to 2.5 natural avalanches in steep high alpine terrain, attributed to wind loading. Cornice failures have also been reported recently, triggering large avalanches. We are also hearing of sluffs in steep solar affected alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A handful of recent large avalanches have been reported over the last few days. Many of these have been on north aspects, with the odd event on other aspects. There has also been a number of cornice falls.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A skier was partially buried in a size 2.5 wind slab on a north aspect at 2600 m on Thursday. Some naturally-triggered wind slabs and cornice falls were also reported. On Wednesday, a naturally-triggered size 2.5 wind slab was observed on a NE aspect at 2500 m. An ice fall also triggered a size 3 deep persistent slab which failed at ground. Human-triggered wind slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported, although I'm sure there has been some smaller wind slab activity in higher elevation lee terrain in response to recent snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We have had no recent reports of avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new today</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday are limited to just one new Size 2 natural wind slab avalanche on a northeast facing alpine slope below a ridge crest. However, reports from Tuesday include several small natural and skier triggered wind slab avalanches in lee and cross-loaded treeline and alpine terrain. The reports mentioned surprisingly little large avalanche activity given the strong winds and amount of fresh snow available for wind-transport.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several cornice falls have been reported in the last few days, some of which have triggered slabs on slopes below.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, a size 2 persistent slab was triggered in a </span><span class="s_2F726580">permanently closed area</span><span class="s_1681A555"> at a ski area. It may have started in the March persistent weak layer before it stepped down to fail at ground.</span><span class="s_71516F31"> While the likelihood of triggering a large persistent slab avalanche has gone down, the consequences remain high.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reported avalanche activity has been limited to small loose dry avalanches spilling out of steep headwalls. Light snowfall and wind forecast for Saturday may result in increased wind slab activity in high elevation lee terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Two reports of large natural avalanches on NE and W aspects from yesterday, and explosive testing by one commercial operator produced a large, 2.5 hard slab avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">There have been several explosive-controlled wind slab avalanches up to Size 2.5 running on facets buried March 25th. On Thursday, a remotely triggered Size 2.5 avalanche released above two skiers catching both of them and burying one, who was successfully recovered. This avalanche failed on the same March 25th weakness, where it was buried surface hoar on a northeast aspect at 1450 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Throughout the week, several natural avalanches size 1.5-3.5 were reported. Some were persistent slabs and some were wind slabs. Persistent slab activity appears to have slowed, but triggering one of these beasts remains a possibility. A few cornice falls were also observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_C6F15715">A size 2.5 slab avalanche was recently reported via the Mountain Information Network. It failed on a surface hoar layer in northeast-facing alpine terrain on Cleveland Peak in White Pass. There has been little in the way of avalanche activity reported at this interface. However, as people venture further afield, there is a greater likelihood of somebody triggering this spotty, yet potentially destructive layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist loose avalanches reported on solar aspects below 1900m.&nbsp; No other reports from the area.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A handful of recent large avalanches have been reported over the last few days. Many of these have been on north aspects, with the odd event on other aspects. There has also been a number of cornice falls.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, sun triggered a few size 2 avalanches in steep terrain. A skier was partially buried in a size 2.5 wind slab on a north aspect at 2600 m on Thursday. Some naturally-triggered wind slabs and cornice falls were also reported. On Wednesday, a naturally-triggered size 2.5 wind slab was observed on a NE aspect at 2500 m. An ice fall also triggered a size 3 deep persistent slab which failed at ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Friday, some loose dry sluffing was reported from steep terrain. On Wednesday, ski cutting produced numerous size 1 wind slabs. On Sunday, it may be possible to trigger new wind slabs in the alpine and exposed areas at treeline. Cornices may be touchy, especially during the heat of the day. Extra caution should be given to all steep south facing slopes when the sun is out during the heat of the afternoon.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations are becoming very limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Thursday, some loose sluffing was reported from steep terrain. On Saturday in the Lizard region, widespread sluffing was reported from steep terrain features and ski cutting produced soft slabs in wind loaded features. On Sunday, it may be possible to trigger new wind slabs in the alpine and exposed areas at treeline. Cornices may become touchy during the heat of the day. If the sun is out during the heat of the afternoon, extra caution should be given to all steep south facing slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of avalanches from the past few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several cornice falls have been reported in the last few days, some of which have triggered slabs on slopes below.</span></p><p class="p_CC664AAA"><span class="s_1681A555">On Wednesday, a size 2 persistent slab was triggered in a </span><span class="s_2F726580">permanently closed area</span><span class="s_1681A555"> at a ski area. It may have started in the March persistent weak layer before it stepped down to fail at ground.</span><span class="s_71516F31"> While the likelihood of triggering a large persistent slab avalanche has gone down, the consequences remain high.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations are becoming more limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Saturday, widespread sluffing was reported from steep terrain features. Ski cutting produced soft slabs in wind loaded features. On Friday, some loose sluffing was reported from steep terrain. On Sunday, it may be possible to trigger new wind slabs in the alpine and exposed areas at treeline. Cornices may become touchy during the heat of the day. If the sun is out during the heat of the afternoon, extra caution should be given to all steep south facing slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent reports of avalanches in the Sea to Sky region</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No recent reports of avalanches have been received</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Throughout the week, several natural avalanches size 1.5-3.5 were reported. Some were persistent slabs and some were wind slabs. Persistent slab activity has slowed, but triggering one of these beasts remains a possibility from a thin spot or with a very large trigger. A few cornice falls were also observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist loose avalanches reported on solar aspects below 1900m. No other reports from the area. Cornices are now becoming a concern as the Spring temps progress</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported from Saturday.  In the days leading up to the weekend a handful of large avalanches were reported, most were from north aspects, with the odd event on other aspects. A number of cornice failures were also observed.</span><span class="s_1681A555" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday storm slabs ran to size 1.5 on NE through NW facing features between 1900 and 2700m. Loose dry avalanches to size 1.5 were reported from all aspects between 2000 and 2500m. A few size wet slabs were reported from southerly facing features between 2100 and 2500m. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">There were a couple noteworthy avalanches from last week. On Thursday a rider was partially buried in a size 2.5 wind slab on a north aspect at 2600m. On Wednesday, a naturally-triggered size 2.5 wind slab was observed on a NE aspect at 2500m. On that same day an ice fall triggered a size 3 deep persistent slab which failed at ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Saturday, explosives triggered small wind slabs and thin storm slabs that ran on a melt-freeze crust.  On Friday and Saturday, natural loose dry sluffing was reported from steep terrain. </span><span class="s_3FE45715">On Monday, it may be possible to trigger new wind slabs in the alpine and exposed areas at treeline. Reverse loading may occur and wind slabs should be expected on all aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations are becoming very limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Thursday, some loose sluffing was reported from steep terrain. On Saturday in the Lizard region, widespread sluffing was reported from steep terrain features and ski cutting produced soft slabs in wind loaded features. On Monday, it may be possible to trigger new wind slabs in the alpine and exposed areas at treeline. Reverse loading may occur and wind slabs should be expected on all aspects. Cornices may become touchy during the afternoon.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Extensive sluffing up to sz 1.5 out of steeper terrain. Moist releases later in the day up to sz 2 on solar aspects.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of avalanches from the past few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several cornice falls have been reported in the last few days, some of which have triggered avalanches on slopes below. On Wednesday, a rider triggered size 2 avalanche was reported that likely started on the March PWL before it stepped down to the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations are becoming more limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Saturday, widespread sluffing was reported from steep terrain features. Ski cutting produced soft slabs in wind loaded features. On Friday, some loose sluffing was reported from steep terrain. On Monday, it may be possible to trigger new wind slabs in the alpine and exposed areas at treeline. Reverse loading may occur and wind slabs should be expected on all aspects. Cornices may become touchy during the afternoon.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports of small size 1 natural avalanches in steep terrain early in the day, then small wet avalanches from solar heating on&nbsp; southern aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No recent reports of avalanches have been received</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday loose dry avalanches to size 1.5 were reported from N/NE features around 1900m. A small cornice failure was observed on a NE facing feature at 2400m. Explosive control work initiated avalanches to size 1.5 on NE through NW facing slopes between 1800 and 2400m. Last week, several persistent and wind slab avalanches to size 3.5 were reported. Persistent slab activity has slowed but cornice failure is ongoing.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist loose avalanches reported on solar aspects below 1900m. No other reports from the area. Cornices are now becoming a concern as the Spring temperatures progress.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A very large (size 3) deep persistent slab failed naturally Sunday on a steep glacial feature at 2500m. It's presumed that this failed on early season basal facets. A small natural cornice fall was also observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reported avalanche activity on Sunday was limited to power sluffing in steep high elevation terrain. On Saturday storm slabs ran to size 1.5 on NE through NW facing features between 1900 and 2700m. Loose dry avalanches to size 1.5 were reported from all aspects between 2000 and 2500m. A few size wet slabs were reported from southerly facing features between 2100 and 2500m. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">There were a couple noteworthy avalanches from last week. On Thursday a rider was partially buried in a size 2.5 wind slab on a north aspect at 2600m. On Wednesday, a naturally-triggered size 2.5 wind slab was observed on a NE aspect at 2500m. On that same day an ice fall triggered a size 3 deep persistent slab which failed at ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Sunday, natural and human-triggered wet sluffing was reported. This was limited to size 1 and was sliding on the late-March crust layer. On Saturday, explosives triggered small wind slabs and thin storm slabs that ran on the crust. With freezing levels rising and lots of sun expected o</span><span class="s_3FE45715">n Tuesday, lots of natural sluffing is expected from steep sun-exposed slopes. Cornices will become weaker than they have been for the last week and may fail naturally. Wind slabs in the alpine are expected to be sensitive to human-triggering. Reverse loading may have occurred and wind slabs should be expected in leeward features on all aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations are becoming very limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. In the Lizard range on Saturday and Sunday, loose sluffing was reported from steep features.&nbsp; Also in the Lizard on Saturday, ski cutting produced small soft slab avalanches in wind loaded features. With freezing levels rising and lots of sun expected on Tuesday, lots of natural sluffing is expected from steep sun-exposed slopes. Cornices will become weaker than they have been for the last week and may fail naturally. Wind slabs in the alpine are expected to be sensitive to human-triggering. Reverse loading may have occurred and wind slabs should be expected in leeward features on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few small loose dry avalanches were observed today on all aspects in steep alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Few reports of loose wet sluffs on solar aspects in the afternoon. Cornices have been getting large and ripe</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several cornice falls have been reported in the last few days, some of which have triggered avalanches on slopes below. On Wednesday, a rider triggered size 2 avalanche was reported that likely started on the March PWL before it stepped down to the ground. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations are becoming more limited as we enter spring. If you're out in the mountains, please consider posting your observations to our webpage. On Saturday and Sunday, loose sluffing was reported from steep features.  On Saturday, ski cutting produced small soft slab avalanches in wind loaded features. With freezing levels rising and lots of sun expected on Tuesday, lots of natural sluffing is expected from steep sun-exposed slopes. Cornices will become weaker than they have been for the last week and may fail naturally. Wind slabs in the alpine are expected to be sensitive to human-triggering. Reverse loading may have occurred and wind slabs should be expected in leeward features on all aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports are beginning to surface of small, loose wet avalanches in steep south facing terrain.  A natural cornice failure  was observed at 2300m on a north aspect, but did not trigger an avalanche</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several large natural avalanches have been reported recently, with one of them being a cornice failure. Solar aspects are becoming active with daytime warming and producing point releases that grow up to size 2, and in one case triggered a slab on a weak layers to size 2.5</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Lot's of cornice failure observed Sunday on NE, NW and even South facing ridge lines. In two separate incidents cornice fall triggered subsequent slab avalanches that ran to size 3 on high elevation terrain features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_C6F15715">A size 2.5 slab avalanche was reported last Friday. It failed on a surface hoar layer in northeast-facing alpine terrain on Cleveland Peak in White Pass. A second size 2 persistent slab avalanche was reported from the same area on Saturday. In the Chilkoot Valley and Haines Junction areas, the buried surface hoar layer has been reported to be very reactive to skier triggering. It seems to be a more isolated problem for the Yukon forecast region. This layer may become more reactive with the storm loading that is expected on Wednesday. On Wednesday and Thursday, touchy new wind slabs are expected to develop. The new snow overlies a new surface hoar layer which may increase the sensitivity of the new slabs. If we get more snow than is currently forecast, a more widespread storm slab problem has the potential to develop.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist loose avalanches have been reported on steep sun-exposed slopes, and one natural cornice fall (size 2) was reported on Monday. This cornice did not trigger a slab on the slope below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new observations from Monday. On Sunday a very large (size 3) deep persistent slab failed naturally on a steep glacial feature at 2500m. It's presumed that this failed on early season basal facets. A small natural cornice fall was also observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday a bit of small loose wet activity was observed. Sunday's observations were limited to power sluffing in steep high elevation terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. With freezing levels rising and lots of sun expected o</span><span class="s_3FE45715">n Wednesday, lots of natural sluffing is expected from steep sun-exposed slopes, especially in areas where cold, dry snow is exposed to solar radiation for the first time. Cornices will become weaker than they have been for the last week and may fail naturally. Wind slabs in the alpine may be sensitive to human-triggering. Reverse loading may have occurred and wind slabs should be expected on a variety of aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. With freezing levels rising and lots of sun expected o</span><span class="s_3FE45715">n Wednesday, lots of natural sluffing is expected from steep sun-exposed slopes, especially in areas where cold, dry snow is exposed to solar radiation for the first time. Cornices will become weaker than they have been for the last week and may fail naturally. Wind slabs in the alpine may be sensitive to human-triggering. Reverse loading may have occurred and wind slabs should be expected on a variety of aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some small isolated loose dry avalanches were noted on polar aspects. Of more concern was a number of loose wet avalanches that started around 2pm. These were much bigger(sz2), and limited to steep alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some loose wet sluffs on solar aspects have been reported in the afternoon. Cornices are getting large and ripe and could pop off with daytime warming. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several cornice falls have been reported in the last few days, some of which have triggered avalanches on slopes below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. With freezing levels rising and lots of sun expected o</span><span class="s_3FE45715">n Wednesday, lots of natural sluffing is expected from steep sun-exposed slopes, especially in areas where cold, dry snow is exposed to solar radiation for the first time. Cornices will become weaker than they have been for the last week and may fail naturally. Wind slabs in the alpine may be sensitive to human-triggering. Reverse loading may have occurred and wind slabs should be expected on a variety of aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent reports include minor pinwheeling or loose wet sluffs in steep sun-exposed terrain. There is also a possibility of cornice falls with daytime warming and intense spring sunshine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday there was a report of a size 2 skier triggered slab and a size 1.5 remotely triggered slab in the northern part of region. These were both from alpine terrain and appeared to fail on a buried surface hoar layer. In the same part of the region a size 3.5 cornice triggered slab was reported from steep unskiable terrain. This likely released on a weakness near the base of the snowpack. Besides these two slabs, the only other reports are of small loose wet sluffs from steep sunny slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Cornice fall continues to occur, failures from NE, NW and even South facing ridge features have been reported over the last few days. In two separate incidents cornice fall triggered subsequent slab avalanches that ran to size 3 on high elevation terrain features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist loose avalanches have been reported on steep sun-exposed slopes, and one natural cornice fall (size 2) was reported on Monday. This cornice did not trigger a slab on the slope below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday cornice failure triggered a size 3 avalanche on a North facing feature at 2700m. No new observations from Monday. On Sunday a very large (size 3) deep persistent slab failed naturally on a steep glacial feature at 2500m. It's presumed that this failed on early season basal facets. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations from Sunday, Monday and Tuesday were limited to power sluffing from steep high elevation terrain and small loose wet activity.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </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">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">With freezing levels rising and lots of sun expected o</span><span class="s_3FE45715">n Thursday, lots of natural sluffing is expected from steep sun-exposed slopes. Cornices will become weaker and may fail naturally. Thin wind slabs may also be sensitive to human triggering on isolated high elevation, lee slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">With freezing levels rising and lots of sun expected o</span><span class="s_3FE45715">n Thursday, lots of natural sluffing is expected from steep sun-exposed slopes. Cornices will become weaker and may fail naturally. Thin wind slabs may also be sensitive to human triggering on isolated high elevation, lee slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few solar triggered sluffs occurred this afternoon up to size 1.5. A few slab avalanches have occurred on steep alpine features on N and E aspects in the past 24 to 36hrs. These generally occurred immediately below cliff bands and ranged between 25 and 50cm deep.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, several loose wet avalanches to size 2 were reported from steep sun-exposed slopes. Some of these did trigger slabs up to size 2.5, potentially releasing on the March 25th surface hoar layer. Observers near the Ningunsaw Pass (northern part of the region) have been reported significant activity on the March 25th interface. For the past few days there have been reports of natural, skier-triggered, and remotely triggered avalanches up to size 3. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several cornice falls have been reported in the last few days, some of which have triggered avalanches on slopes below. Small loose wet avalanches running in the storm snow from last weekend have also been observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">With freezing levels rising and lots of sun expected o</span><span class="s_3FE45715">n Thursday, lots of natural sluffing is expected from steep sun-exposed slopes. Cornices will become weaker and may fail naturally. Thin wind slabs may also be sensitive to human triggering on isolated high elevation, lee slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent reports include minor pinwheeling or loose wet sluffs in steep sun-exposed terrain. There is also the potential for cornice falls with daytime warming and intense spring sunshine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Note: Almost all of the recent reported activity is from the Northern part of the region near Ningunsaw Pass. This could be because this is the hot spot at the moment, but it could also be because there are few observers in the field further south. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">For the past few days, there have been reports of natural, skier-triggered, and remotely triggered slabs up to size 3 releasing on the March 25th surface hoar layer. Some of these have been triggered from below or in low-angle terrain. In addition, cornices have been failing and loose wet activity has been noted in the afternoon, both of which have triggered deeper persistent slabs. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Cornice failures from almost all aspects continue to be observed. In two recent incidents cornice fall triggered subsequent slab avalanches that ran to size 3 on high elevation terrain features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Moist loose avalanches have been reported on steep sun-exposed slopes, and one natural cornice fall (size 2) was reported earlier in the week, but didn't trigger a slab release on the slope below. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A few natural cornice failures were observed Wednesday, but slabs were only triggered in steep, unsupported rocky features and even then had minimal propagation. On Tuesday cornice failure triggered a size 3 avalanche on a North facing feature at 2700m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday loose wet avalanches averaged size 1, with a size 2.5 being reported from steep rocky terrain. Observations from Sunday, Monday and Tuesday were limited to power sluffing from steep high elevation terrain and small loose wet activity.</span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose wet avalanches to size 1.5 have been reported in this region recently. This kind of activity is likely to continue through Friday, although the intensity may diminish a little bit on account of less solar radiation and slightly cooler temperatures. Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network.</span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet avalanches to size 1.5 were reported from neighboring forecast regions (Lizard-Flathead and Waterton National Park) on Tuesday and Wednesday. This kind of activity is likely to be seen in this region through Friday, although the intensity may diminish just a little on account of less solar radiation and slightly cooler temperatures.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Solar triggerred avalanches are becomming more the norm at this time of year.  Loose wet slides and potentially loose wet slabs are likely.  There may even be a combination of both of these with loose wet slides triggerring slabs on the underlying slopes.  These wet avalanches tend to be slow moving but very destructive reaching well down into normal runouts.  Keep an eye on the terrain you are on, and travelling under.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose wet avalanches to size 2 have been reported from steep sun-exposed slopes. Some of these triggered slabs up to size 2.5, possibly releasing on the March 25th surface crust/ surface hoar layer. Observers near the Ningunsaw Pass (northern part of the region) have reported significant activity on the March 25th interface. For the past few days there have been reports of natural, skier-triggered, and remotely triggered avalanches up to size 2.5. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several cornice falls have been reported in the last few days, some of which have triggered slabs on slopes below, some which have not. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Loose wet avalanches to size 1.5 were reported on Tuesday and Wednesday. This kind of activity is likely to continue through Friday, although the intensity may diminish a little bit on account of less solar radiation and slightly cooler temperatures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent reports include minor pinwheeling or loose wet sluffs in steep sun-exposed terrain. There is also the potential for cornice falls with daytime warming and intense spring sunshine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">For the past few days, there have been reports of natural, skier-triggered, and remotely triggered slabs up to size 2.5 releasing on the March 25th surface hoar layer. Some of these have been triggered from below or in low-angle terrain. In addition, cornices have been failing and loose wet activity has been noted in the afternoon, both of which have triggered deeper persistent slabs. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural cornice failures continue to be observed in the alpine on almost all aspects. In two recent incidents cornice fall triggered subsequent slab avalanches that ran to size 3 on high elevation terrain features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Little in the way of avalanche activity from yesterday.  Moist loose avalanches had been reported earlier in the week, but with falling temperatures this activity has gone dormant. Expect wind slab activity with new loading and strong winds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A few natural cornice failures were observed Wednesday &amp; Thursday, but slabs were only triggered in steep, unsupported rocky features and even then had minimal propagation. On Tuesday cornice failure triggered a size 3 avalanche on a North facing feature at 2700m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In two separate incidents Thursday cornice fall triggered deep persistent slabs when it impacted slopes below. Both incidents were on north facing alpine features. Loose wet avalanches to size 2 were also observed from south through west facing terrain. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network.&nbsp; </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose wet avalanches to size 1.5 were reported from neighboring forecast regions (Lizard-Flathead and Waterton National Park) during warm periods through this week. This kind of activity is likely to be seen in this region when the sun comes out and/or temperatures become warm. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network.</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">In the past week, loose wet avalanches to size  2 were reported to have triggered slabs up to size 2.5, possibly releasing on the March 25th surface crust/ surface hoar layer. No reports of avalanches from yesterday, but one commercial operator reports that strong winds are stripping new snow down to the old crust surface and depositing it on lee slopes as windslabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several cornice falls have been reported in the last few days, some of which have triggered slabs on slopes below, some which have not. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches have been reported. </span></p><p class="p_CC664AAA"><span class="s_AA239A9B">Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Snowballing and/or pin-wheeling on solar aspects was the last acivity reported during the warm clear spell of weather that just finished. Expect wind slab activity and cornice failures with the current weather pattern and increased loading.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reported avalanche observations from yesterday, but commercial operators reported strong winds in the alpine stripping the new snow down to old crust surfaces and building wind slabs and sastrugi.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural cornice failures continue to be observed in the alpine on almost all aspects. Recently a size 3 cornice failure did not propagate a slab when it impacted the steep north facing slope below. Numerous loose snow avalanches to size 2 were reported as the strong spring sun shined on solar facing slopes Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several naturally-triggered loose snow avalanches were observed on steep east to south-facing aspects on Friday. In some areas, these pulled out small storm slabs. Poor weather kept observers from seeing what was going on up high, where snowfall and wind-loading has probably been more intense.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of avalanche activity from yesterday.  This is most likely as a result of few field observations. We expect wind slab activity with new loading and strong winds.  Solar aspect may become active again when the sun come out.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new activity to report from Friday. A few natural cornice failures were observed Wednesday &amp; Thursday, but slabs were only triggered in steep, unsupported rocky features and even then had minimal propagation. On Tuesday cornice failure triggered a size 3 avalanche on a North facing feature at 2700m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new activity to report from Friday. In two separate incidents Thursday cornice fall triggered deep persistent slabs when it impacted slopes below. Both incidents were on north facing alpine features. Loose wet avalanches to size 2 were also observed from south through west facing terrain. </span></p><p class="p_CC664AAA"><span class="s_3FE45715"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Loose wet avalanches to size 1.5 have been reported in this region recently. Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2 loose wet slide was reported in the Lizard Range on Friday. Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network.</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 few loose dry avalanches were observed from steeper terrain on Saturday.  Also there was a report of a sz 2.5 on a N aspect near the &quot;Sharks tooth&quot; peak in the commonwealth area.  This avalanche was likely triggered by a cornice collapse. </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">No reports of natural avalanche activity yesterday, most likely because of few observations during this storm, but one operator has reported good results, up to size 2.5, with explosives in wind loaded terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several cornice falls have been reported in the last few days, some of which have triggered slabs on slopes below, some which have not. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">One size 2 loose wet slide was reported from a North aspect on Friday, and several other size 1-1.5 loose sluffs were reported earlier in the week. Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network.</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">No reports of avalanche activity in the Sea to Sky region, (yet..), probably because the storm is just beginning. Expect wind slab activity and cornice failures with the current weather pattern and increased loading. Solar aspects will be come active when the sun comes out.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Commercial operators are reporting strong winds in the alpine stripping the new snow down to old crust surfaces and building wind slabs and sastrugi. One operator has reported numerous size 2 and 2.5 avalanches with explosives control.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural cornice failures continue to be observed in the alpine on almost all aspects. Recently a size 3 cornice failure did not propagate a slab when it impacted the steep north facing slope below. Numerous loose snow avalanches to size 2 were reported as the strong spring sun shined on solar facing slopes Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of avalanche activity from yesterday. This is most likely as a result of few field observations. We expect wind slab activity with new loading and strong winds. Solar aspects will become active again when the sun come out, and cornices will again be on our radar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new observations have been received but this is due to a lack of observers. On Saturday in the North Columbia region, isolated natural avalanche activity was reported up to size 2.5. Skiers and explosives also triggered avalanches up to size 1.5. These were mainly storm slabs with thickness of 30-40cm. The Cariboo region received less snowfall so wind slabs may be a bigger problem than storm slabs. </span><span class="s_3FE45715">On Monday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features.  If the sun is out in the afternoon, extra caution should be given to steep sun-exposed slopes.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, isolated natural avalanche activity was reported up to size 2. Skiers and explosives also triggered avalanches up to size 1.5. These were mainly storm slabs with thickness of 10-30cm. One wind slab was reported to have been triggered remotely from 30m away suggesting that the weak layer is very reactive in some areas. On Monday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. If the sun is out in the afternoon, extra caution should be given to steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Only minor pinwheeling and loose snow slides have been observed in the past couple days. Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple size 1-1.5 loose snow slides were reported from neighbouring regions on Saturday. Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network.</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">No new avalanche activity was observed on Sunday but observations were limited due to visibility.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of natural avalanche activity yesterday, most likely because of few observations during this storm, but one operator recently reported good results, up to size 2.5, with explosives in wind loaded terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, isolated natural avalanche activity was reported up to size 2 in the north of the region. Skiers also triggered avalanches up to size 1.5. These were mainly storm slabs with thickness of 15-40cm. One storm slab was reported to have been triggered remotely from 30m away suggesting that the weak layer is very reactive in some areas. On Monday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. If the sun is out in the afternoon, extra caution should be given to steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new observations from the region, but neighbouring regions reported a few size 1-1.5 loose snow avalanches on Saturday. Observations are becoming more limited as we enter into spring. If you're out in the mountains, please consider posting your observations to our webpage using the Mountain Information Network.</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">Explosive control yesterday produced numerous 1 to 1.5 soft slab avalanches.&nbsp; Commercial operators are noting soft slabs in lee terrain.&nbsp; Not many observations reported, mostly as a result of poor visibility during the storm cycle.  We expect wind slab activity and cornice failures with the current weather pattern and increased loading, as well as loose-wet avalanches on solar aspects when the sun comes out.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of natural or skier / rider triggered avalanche in the past few days, probably because of the storm cycle and lack of visibility for field observations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, isolated natural avalanche activity was reported up to size 2.5. Skiers and explosives also triggered avalanches up to size 1.5. These were mainly storm slabs with thickness of 30-40cm. One storm slab was reported to have been triggered remotely from 50m away suggesting that the weak layer is very reactive in some areas. On Monday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. If the sun is out in the afternoon, extra caution should be given to steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of avalanche activity from yesterday. This is most likely as a result of few field observations. I suspect wind slab activity with new loading and strong winds and solar aspects may become active again when the sun come out. Watch overhead hazards like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported in the Cariboos but this is mainly due to a lack of observers. On Sunday in the North Columbia region where conditions are expected to be similar, natural storm slab activity was reported up to size 2.5 and several remotely triggered avalanches were reported with the furthest being triggered from 200m away. This suggests that the weak layer below the storm slab is very reactive in some areas. On Tuesday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. If the sun is out in the afternoon, natural avalanche activity is expected and extra caution should be given to steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, natural avalanches up to size 2.5 were reported.  Slabs were typically 30-50cm thick and were occurring above 2000m elevation.  Two remotely triggered avalanches have been reported and were triggered from up to 30m away. These remote triggers as well as reports of whumphing and wide propagations are suggesting that the weak layer below the storm snow is very reactive in some areas.  On Saturday, isolated natural avalanche activity was reported up to size 2 and skiers/explosives triggered avalanches up to size 1.5. </span><span class="s_3FE45715">On Tuesday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. If the sun is out in the afternoon, natural avalanche activity is expected and extra caution should be given to steep sun-exposed slopes.</span><span class="s_3FE45715" /></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">One isolated slab was noted below a cliff in the alpine, sz1.5 on an east aspect. Late day loose wet avalanches are suspected on steep solar aspects. Forecasters left the field before the heat of the day reached its peak. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of natural avalanche activity yesterday. With continued precipitation, localized solar radiation and strong winds new storm slabs and winds slabs will likely be touchy on Tuesday. Natural and human triggered avalanches up to size 2 are expected. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, skiers and explosives triggered storm slabs up to size 2.5. Typical slab depths were 40-60cm but slabs up to 80cm were reported in wind loaded areas. Multiple remotely triggered avalanches were reported with the furthest being triggered from 100m away. This suggests that the weak layer below the storm slab is very reactive in some areas. On Saturday, isolated natural avalanche activity was reported up to size 2 in the north of the region and skiers triggered avalanches up to size 1.5. On Tuesday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. If the sun is out in the afternoon, natural avalanche activity is expected and extra caution should be given to steep sun-exposed slopes.</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_3FE45715">Reports of a human triggered size 2 storm slab was remotely triggered 15 m away. There was no personal involvement, however the slab did fail on facets above a crust which was buried on April 10th. Explosive control work triggered several size 1.5 loose dry avalanches and no new naturals were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent explosive control has produced loose dry avalanches up to size 1.0. With continued snow, rain, and strong winds natural avalanche activity will occur on Tuesday, touchy wind slab and storm slab avalanches size 2 or greater will likely be the primary concern. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, natural storm slab activity up to size 2.5 was reported.  Several remotely triggered avalanches were reported to be triggered from up to 200m away.  This suggests that the weak layer below the storm slab is very reactive in some areas.  The slab avalanches that were reported were typically 40-60cm thick. On Saturday, isolated natural avalanche activity was reported up to size 2.5 and skiers/explosives also triggered avalanches up to size 1.5. On Tuesday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. If the sun is out in the afternoon, natural avalanche activity is expected and extra caution should be given to steep sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There are a couple recent observations of size 1-2 natural wind slabs from North facing alpine slopes. These were typically 30-50 cm deep. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of avalanche activity from yesterday. This is most likely as a result of few field observations. I suspect wind slab activity with new loading and strong winds and solar aspects may become active again when the sun come out. Watch overhead hazards like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a cornice triggered a size 1.5 avalanche in the Valemont area. This was 40cm deep and released on the mid-April weak layer. Around Blue River, a cornice was intentionally released but the cornice failure did not trigger a slab on the slope below. In this area where the storm snow amounts are less, wind slabs in specific areas are the biggest concern whereas deeper areas can expect a more widespread storm slab problem. In the North Columbia region, more widespread activity has been reported including natural and skier-triggered avalanches up to size 2.5. Remotely triggered avalanches have been reported from up to 200m away which suggests that the weak layer below the storm snow is very reactive in this region. On Wednesday, lingering storm slabs or wind slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. The sun is expected to trigger some natural activity on steep solar aspects including both loose wet avalanches and slab avalanches. Cornices will become weak in the afternoon and natural cornice falls have the potential to trigger large slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, isolated natural avalanches were reported as well as several skier triggered avalanches. These storm slabs were typically 30-50cm thick and were generally occurring above 2100m elevation. A couple small wet avalanches were reported from lower elevations. Several remotely triggered avalanches have been reported over the last 3 days and were triggered from up to 60m away. These remote triggers as well as reports of whumphing and wide propagations are suggesting that the weak layer below the storm snow is very reactive in some areas. Over the weekend, natural, human-triggered, and explosive-triggered storm slab avalanches up to size 2.5 were ongoing. Towards the southern parts of the region that received less recent snowfall, wind slabs in specific areas have been the primary concern. On Wednesday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. The sun is expected to trigger natural activity on steep solar aspects including both loose wet avalanches and slab avalanches. Cornices will become weak in the afternoon and natural cornice falls have the potential to trigger large slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported. On Wednesday, touchy wind slabs and storm slabs are likely, especially in areas that receive higher snowfall amounts or localized solar radiation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, ski cutting produced a size 1.5 avalanche with a depth of 25cm.  Explosives triggered a cornice which triggered two size 2 slabs on the slope below.  These were 40cm thick slabs and failed on a north aspect.  On Sunday, skiers and explosives triggered storm slabs up to size 2.5. Typical slab depths were 40-60cm but slabs up to 80cm were reported in wind loaded areas. Multiple remotely triggered avalanches were reported with the furthest being triggered from 100m away. This suggests that the weak layer below the storm slab is very reactive in some areas. On Saturday, isolated natural avalanche activity was reported up to size 2 in the north of the region and skiers triggered avalanches up to size 1.5. On Wednesday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. The sun is expected to trigger some natural activity on steep solar aspects including both loose wet avalanches and slab avalanches. Cornices will become weak in the afternoon and natural cornice falls have the potential to trigger large slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent observations. On Monday, no natural activity was reported but numerous size 1 storm slabs were easily triggered by the weight of a skier, especially in areas that saw some wind effect. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, explosive control showed numerous storm slab and wind slab avalanches up to size 2. These were primarily from N-NW aspects above 1300 m. With continued snow, rain, and strong winds natural avalanches and human triggered avalanches will likely continue on Wednesday. Lower elevations which have become rain soaked may see natural loose wet avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a couple size 1.5 skier triggered avalanches were reported. Over the weekend, natural, human-triggered, and explosive-triggered storm slab avalanches up to size 2.5 were ongoing. Storm slabs were typically 30-50cm thick. Several remotely triggered avalanches have been reported over the last 3 days and were triggered from up to 200m away. These remote triggers as well as reports of whumphing and wide propagations are suggesting that the weak layer below the storm snow is very reactive in some areas. On Wednesday, lingering storm slabs are expected to be reactive to human-triggering, especially in steep alpine terrain and wind-loaded terrain features. The sun is expected to trigger some natural activity on steep solar aspects including both loose wet avalanches and slab avalanches. Cornices will become weak in the afternoon and natural cornice falls have the potential to trigger large slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No reports of avalanche activity from yesterday. This is most likely as a result of few field observations. I suspect wind slab activity with new loading and strong winds. Strong solar radiation and warming expected on Thursday will likely initiate a natural avalanche cycle. Watch overhead hazards like cornices.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, natural storm slabs up to size 2.5 were reported around Blue River and Valemont. These slabs had depths from 20-80cm. Ski cuts triggered a couple size 2 wind slabs with 20cm thickness. A remotely triggered avalanche was triggered from 10m away. Remote triggering suggests the weak layer below the storm snow has been very reactive in some areas. On Monday, a natural cornice release triggered a size 1.5 slab avalanche on the slope below. Solar triggered slab avalanches, cornice releases, and loose wet sluffing are all expected to have occurred on Wednesday. With overcast conditions expected on Thursday and a new surface crust expected to form Wednesday night, stability should begin to improve. Human-triggering remains a major concern at higher elevations, especially north facing terrain where the storm slab is unaffected by the sun on Wednesday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a natural cornice failure triggered a size 2 slab avalanche on the slope below. Three size 1-1.5 skier triggered avalanches were also reported. Two of these were triggered remotely with the furthest being triggered from 100m away. Several remotely triggered avalanches have been reported recently as well as whumphing and wide propagations. These indicate that the weak layer below the storm snow has been very reactive in some areas. Over the weekend, natural, human-triggered, and explosive-triggered storm slab avalanches up to size 2.5 were ongoing. Towards the southern parts of the region that received less recent snowfall, wind slabs in specific areas have been the primary concern. Solar triggered slab avalanches, cornice releases, and loose wet sluffing are all expected to have occurred on Wednesday. On Thursday, the same types of solar related activity are expected. If a supportive crust forms Wednesday night, stability will begin to improve. Human-triggering remains a major concern at higher elevations, especially north facing terrain where the storm slab is unaffected by the sun on Wednesday. </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">Loose wet on solar aspects up to sz1.5 and cornice collapses were noted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanches aren't expected at this time. Forecast bulletins still exist for neighboring regions until Sunday April 19th. Beyond that, to assist with your backcountry travel planning we've produced blog posts describing four common spring scenarios. It's up to you to decide which of the scenarios applies to your situation. Each scenario has specific weather, snowpack, and avalanche characteristics. And each requires a different approach in terms of risk management. Click the link in the bulletin headline for more information on these different spring scenarios.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported. On Thursday, touchy wind slabs and storm slabs are likely, especially in areas that receive higher snowfall amounts or localized intense solar radiation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, skiers and explosives triggered storm slab avalanches size 1-2.  These were 30-60cm thick slabs on north through east aspects in the alpine.  Explosives were also used to trigger a cornice release which subsequently triggered a size 3 slab avalanche that may have stepped down to a deeper layer in the snowpack.  A skier also remotely triggered a storm slab avalanche from 30m away.  Several remotely triggered avalanches have been reported in the last few days from up 100m away as well as whumphing and wide propagations.  This suggests that the weak layer below the storm slab has been very reactive in some areas.  Over the weekend, isolated natural avalanche activity up to size 2.5 was reported as well as skier triggered avalanches up to size 1.5. Solar triggered slab avalanches, cornice releases, and loose wet sluffing are all expected to have occurred on Wednesday. On Thursday, the same types of solar related activity are expected. If a supportive crust forms Wednesday night, stability will begin to improve. Human-triggering remains a major concern at higher elevations, especially north facing terrain where the storm slab is unaffected by the sun on Wednesday. </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_3FE45715">On Tuesday, a skier triggered size 1 storm slab avalanche failed on a NE aspect around 2100 m. The skier was partially buried with no injuries. The avalanche was anywhere from 10-40 cm deep, 10 m wide and 10 m long. Natural loose wet avalanches occurred up to size 1.5 from steep solar aspects and an explosive triggered size 2 cornice failed, which entrained the recent storm snow but did not pull a slab. With warming and periods of intense solar radiation, persistent slabs may re-awaken, weak cornices will likely fail and loose wet avalanches will continue. Be aware of rapidly changing conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a natural cycle up to size 3 was reported from steep alpine and treeline terrain. Suspect some of these naturals are stepping down to the old interfaces buried April 9 th and mid- March. Explosive control showed numerous storm slab and wind slab avalanches up to size 2.5. These were primarily from NW-N-E aspects above 1400 m. With continued snow, rain, and strong winds natural avalanches and human triggered avalanches will likely continue on Thursday. Lower elevations which have become rain soaked and natural loose wet avalanches from steeper terrain features are expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, natural storm slab avalanches size 2-3 were reported. A ski cut produced a size 1.5 slab release and skiers were triggering dry sluffing in the alpine. Over the weekend, natural, human-triggered, and explosive-triggered storm slab avalanches up to size 2.5 were ongoing. Several remotely triggered avalanches have been reported over the last few days and were triggered from up to 200m away. These remote triggers as well as reports of whumphing and wide propagations are suggesting that the weak layer below the storm snow has been very reactive in some areas. Solar triggered slab avalanches, cornice releases, and loose wet sluffing are all expected to have occurred on Wednesday. On Thursday, the same types of solar related activity are expected. If a supportive crust forms Wednesday night, stability will begin to improve. Human-triggering remains a major concern at higher elevations, especially north facing terrain where the storm slab is unaffected by the sun on Wednesday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Soft slabs are developing in lee and cross loaded alpine and treeline features. These are sitting over variable hard surfaces. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No activity was noted.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches have been reported. Thin new storm slabs may develop with forecast snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. I suspect that new storm slabs are bonding poorly in some areas and may be easy to trigger with light additional loads.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. New storm slabs are expected to develop that may not bond well to the old surfaces.</span><span class="s_1681A555" /></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches reported. I suspect that new storm slabs are developing and may be easily triggered by light additional loads.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We have not received any reports of avalanches on Tuesday, however; more snow, rain and strong winds make the perfect recipe for natural avalanche activity. I'd suspect storm and wind slab avalanche activity at higher elevations and loose wet avalanches at lower elevation. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural loose dry avalanches from size 1.5 to 2 were reported from alpine features facing North, Northeast, East and and Southeast over the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The only recent avalanche activity reported has been loose snow sluffing from steep north facing terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No avalanche activity has been reported from the Cariboos for days. If you have observed any, please share your information through the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A size 1 wind slab failed naturally on a buried rain crust yesterday. With new snow and strong winds, I'd expect avalanche danger to be on the rise at the latter end of this forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. This may speak to the lack of observations rather than actual conditions. With new snow and strong winds forecast the avalanche danger will likely be on the rise.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. If you are out in the mountains, please post your observations to the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Expect small slab development in lee alpine features today after several days of no avalanche activity observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent reports or observations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches have been reported. Thin new storm slabs are expected to develop with forecast snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. I suspect that new storm slabs are bonding poorly in some areas and may be easy to trigger with light additional loads.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. I suspect that new storm slabs are bonding poorly in some areas and may be easy to trigger with light additional loads.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. However, new wind slabs may develop with strong winds and rising freezing levels. Watch loose dry avalanches from steeper terrain features. If you are out in the mountains, please post your observations to the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. I suspect that new storm slabs are developing and may be easily triggered by light additional loads</span><span class="s_1681A555">.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported on Wednesday. With new snow and strong winds, and possible rising temperatures, I'd expect avalanche danger to be on the rise at the latter end of this forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. This may speak to the lack of observations rather than actual conditions. With new snow and strong winds forecast the avalanche danger will likely be on the rise. I'd suspect loose dry avalanches especially from steeper terrain, and storm slab developments at upper elevations. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We have not received any reports of avalanches on Wednesday, however; more snow, rain and strong winds make the perfect recipe for natural avalanche activity where enough snow exists. I'd suspect storm and wind slab avalanche activity at highest elevations and loose wet avalanches at lower elevation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural loose dry avalanches from size 1.5 to 2 were reported from alpine features facing North, Northeast, East and and Southeast over the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Control work Tuesday produced shallow loose dry avalanches to size 2 on W through NE facing features at treeline.  No other activity reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural and skier triggered loose, moist size one avalanches were observed at treeline on Thursday morning. Moist slabs to size 2 are likely with light triggers from alpine start zones. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity has been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, skiers triggered numerous small loose sluffs and soft slabs, even from a distance away. Their reactivity was described as electric. As the snow load builds, I expect a more widespread cycle to kick off. A naturally triggered size 2 slab failed on a SE aspect at 2000 m on Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanche activity has been reported, but I expect a natural avalanche cycle is already underway in areas with the heaviest new snow and/or wind effect. I would anticipate avalanche sizes to go up through the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanche activity has been reported, but I expect a natural avalanche cycle is already underway in areas with the heaviest new snow and/or wind effect. Cracking and whumpfing was reported with around 15 cm of new snow today. As the load builds, I expect a natural cycle to kick off (by late Thursday in many places). I expect avalanche sizes to go up through the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. New snow combined with strong winds is the perfect recipe for the avalanche danger to rise. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural loose wet and wet slab avalanches have been reported below 1800 metres where heavy rain soaked the snowpack. I suspect there are no alpine observations due to poor travel conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. With new snow, strong winds, and possible rising temperatures, I'd expect avalanche danger to be on the rise at the latter end of this forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. If you are out in the mountains, please post your observations to the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches have been reported. Thin new storm slabs are expected to develop with forecast snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. New storm slabs should settle over night and forecast cooler temperatures may help improve stability.</span><span class="s_1681A555" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural and skier triggered loose, moist size one avalanches were observed at treeline on Thursday morning. Moist slabs to size 2 are likely with light triggers from alpine start zones. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. If you are out in the mountains, please post your observations to the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity has been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, numerous small loose sluffs and soft slabs were triggered naturally and by skiers, even from a distance away. Their reactivity was described as electric. As the snow load builds, I expect a more widespread cycle to kick off. A naturally triggered size 2 slab failed on a SE aspect at 2000 m on Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanche activity has been reported, but I expect a natural avalanche cycle is already underway in areas with the heaviest new snow and/or wind effect. I would anticipate avalanche sizes to go up through the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A size 2 storm slab failed on a SE aspect. Several small loose wet avalanches were observed below the rain line (1200 m) yesterday. We don't have a lot of information from field observers yet, but I expect this type of activity was more widespread.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday reports indicated a surprisingly lack of avalanches, this could be due to lack of visibility. I suspect storm slabs are touchy and natural avalanches are likely through the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural avalanche activity occurred during the Thursday storm. Areas that did not slide continue to be suspect. New storm slabs are expected to develop on Saturday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No recent avalanches have been reported. Thin new storm slabs are expected to develop with forecast snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosive controlled storm slab avalanches up to size 2.5 and skier controlled cornice to size 2.0 on Thursday from north of Stewart. No new natural avalanches reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle ran from most start zones below 2200 meters on Thursday. Explosive testing on Friday triggered a single size 2.5 slab that stepped down to the interface buried on December 2nd.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">One small isolated loose dry avalanche was observed in the alpine from steep unskiable terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, a natural size 3.5 was reported from a steep NE aspect at 2100m.  This was a wind loaded start zone and the slab was 60cm thick.  Ski cutting also produced a size 1 storm slab with a 50cm thick slab.&nbsp; If we get the forecast snowfall amounts Saturday night, I expect the storm slab to become a widespread problem on Sunday. The slab will likely be very sensitive to human-triggering at all elevations, especially on steep, convex features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, numerous natural and human-triggered avalanches were reported up to size 2.  Most of this activity was reported at below treeline elevation on a variety of aspects.  If we get the forecast snowfall amounts Saturday night, I expect the storm slab to become a widespread problem on Sunday.  The slab will likely be very sensitive to human-triggering at all elevations, especially on steep, convex features. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports of loose wet natural avalanches at lower elevations and numerous explosive controlled storm slabs up to size 2.5</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No reports of avalanche activity in the forecast region</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No reports of natural activity in the forecast region, but Explosive controlled storm slab avalanches up to size 2.5 and skier controlled cornice to size 2.0 on Thursday from north of Stewart. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Recent reports of a number of size 1.5 natural-cornice failures have been reported through the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We're receiving limited reports from the region and visibility has been poor. Recent observations suggest that the storm snow is becoming reactive as a soft slab, at least on convex features. No further details available.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, explosives triggered a size 2.5 deep persistent slab avalanche in the Dogtooth. This was triggered in a steep, rocky, and unsupported terrain feature and released on the crust/facet interface on the ground. Other explosives resulted in thin wind slabs releasing. If enough snow falls Saturday night, the storm problems may become more widespread. In the deepest western parts of the region (Bugaboos/Bobbie Burns areas), the hazard may be higher if the storm slabs exceed 30-40cm thickness.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Friday, numerous natural and human-triggered avalanches were reported up to size 2.  Most of this activity was below treeline on a variety of aspects.  Natural and human triggered avalanche activity is expected to increase Sunday with the incoming storm Saturday night.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. If you are out in the mountains, please post your observations to the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday control work produced small storm slabs on north through east facing features above 1600m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Easily triggered size one soft slab avalanches have been observed over the last two days. Isolated deep slabs have been triggered with explosive testing above 2200 meters. These deeper slabs stepped down into old layers. Expect skier triggered size two wind affected slabs from lee start zones for the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new Natural avalanches were observed. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm. On Friday, a natural size 3.5 was reported from a steep NE aspect at 2100m. This was a wind loaded start zone and the slab was 60cm thick. Ski cutting also produced a size 1 storm slab with a 50cm thick slab. On Saturday. several natural size 1 avalanches were reported from below treeline elevation. On Monday, touchy storms slab will continue to be very sensitive to human-triggering at all elevations, especially on steep, convex features. Widespread natural avalanche activity is also expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday and Saturday, numerous natural and human-triggered avalanches were reported up to size 2. These avalanches occurred at all elevations and aspects. On Monday, touchy storms slab will continue to be very sensitive to human-triggering at all elevations, especially on steep, convex features. Widespread natural avalanche activity is also expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday natural storm slab avalanches to size 2 were reported on East, North, and Northwest facing features between 1900 and 2100m. These were likely running on the early December surface hoar. Late Sunday we received a report from the Rossland range where a group of skiers triggered a size 2.5 avalanche on a north facing piece of terrain at 1700m. The avalanche initially failed at the Mid-November crust before stepping down to the ground. Thankfully, it sounds like everyone involved will be okay.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, explosives triggered a size 2.5 deep persistent slab avalanche in the Dogtooth. This was triggered in a steep, rocky, and unsupported terrain feature and released on the crust/facet interface on the ground. Other explosives resulted in thin wind slabs releasing. On Monday, storms slab will continue to build and are expected to become sensitive to human-triggering at all elevations, especially on steep, convex features. Natural avalanche activity is also expected to increase in frequency.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday control work produced small storm slabs on north through east facing features above 1600m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. If you are out in the mountains, please post your observations to the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Limited observations due to the current storm cycle. A few reports of soft slabs, storm snow running on previous storm surface up to size 1.5, North aspect around treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No avalanche activity has been reported in the forecast region</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> No reports of natural activity in the forecast region, but Explosive controlled storm slab avalanches up to size 2 and skier controlled cornice to size 2.0 on Thursday from north of Stewart.&nbsp; Operators are reporting sluffing in steep terrain in the new storm snow at tree line and below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A number of size 1.5 natural, cornice failures were reported earlier in the week observed in the Duffey lake region. No other reports of avalanches</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, several natural avalanches were reported up to size two, at treeline and below, on all aspects. Natural avalanching likely occurred in the alpine, but was not observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Easily triggered size 1-2 soft slab avalanches have been observed over the last few days. Most have been running within the storm snow layers but a few isolated slabs have failed on the November 18th crust.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new was observed today, but visibility was limited.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There have been reports of a widespread natural avalanche activity from the Whistler area that is likely indicative of what is going on in the rest of the Sea to Sky region. This cycle is expected to continue as a series of storms pummels the coast range over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">A widespread avalanche cycle is expected to continue as a series of storms pummels the coast range over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Recent reports of natural, rider and remotely triggered avalanches from the mountains around Shames suggest that the load on a layer of recently buried surface hoar has reached critical levels.</span><span class="s_1681A555" /></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">It sounds like there were touchy conditions out there over the weekend.   Reports of some large skier triggered and skier controlled avalanches from tree-line suggest that the load on the recently buried surface hoar is reaching critical levels</span><span class="s_E5CBE62C">.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday and Sunday, several natural and human-triggered avalanches were reported up to size 2. These storm slabs were typically 50-80cm thick and occurred on all aspects and elevation bands. Of particular concern on Sunday were three remotely triggered avalanches, the furthest being triggered from 150m away. This suggests that the storm slab is gaining cohesion and the propagation potential of the underlying weak layer is increasing. On Tuesday, touchy storms slab will continue to be very sensitive to human-triggering at all elevations. Remote-triggering remains a serious concern, especially below 1800m where the surface hoar layer is most reactive. Widespread natural avalanche activity is also expected with the forecast heavy precipitation and rising freezing levels. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday and Sunday, several natural and human-triggered avalanches were reported up to size 2. These storm slabs were typically 50-80cm thick and occurred on all aspects and elevation bands. Of particular concern on Sunday were a couple remotely triggered avalanches, the furthest being triggered from 40m away. This suggests that the storm slab is gaining cohesion and the propagation potential of the underlying weak layer is increasing. On Tuesday, touchy storms slab will continue to be very sensitive to human-triggering at all elevations. Remote-triggering remains a serious concern, especially below 1800m where the surface hoar layer is most reactive. Widespread natural avalanche activity is also expected with the forecast heavy precipitation and rising freezing levels.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been very limited during the storm. On Friday, a natural size 3.5 was reported from a steep NE aspect at 2100m. This was a wind loaded start zone and the slab was 60cm thick. Ski cutting also produced a size 1 storm slab with a 50cm thick slab. On Saturday, several natural size 1 avalanches were reported from below treeline elevation. On Sunday, a ski cut produced a size 1 on a NE aspect at 2000m with a 30cm thick storm slab. In the Northern Monashees, an avalanche was remotely triggered from 150m away.&nbsp; This suggests that the storm slab is gaining cohesion and the propagation potential of the underlying weak layer is increasing. On Tuesday, touchy storms slab will continue to be very sensitive to human-triggering at all elevations. Remote-triggering remains a serious concern, especially below 1800m where the surface hoar layer is most reactive. Widespread natural avalanche activity is also expected with the forecast heavy precipitation and rising freezing levels.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, explosives triggered a size 2.5 deep persistent slab avalanche in the Dogtooth. This was triggered in a steep, rocky, and unsupported terrain feature and released on the crust/facet interface on the ground. Other explosives resulted in thin wind slabs releasing. On Sunday, explosives triggered storm slabs up to size 2 which were typically 20-40 cm thick. In the Selkirks to the west, three remotely triggered avalanches were reported, the furthest being triggered from 150m away. This suggests that the storm slab is gaining cohesion and the propagation potential of the underlying weak layer is increasing. On Tuesday, touchy storms slab will continue to be very sensitive to human-triggering at all elevations. Remote-triggering may also become a concern, especially below 1800m where the surface hoar layer is most reactive. Natural avalanche activity is also expected with the forecast heavy precipitation and rising freezing levels.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. If you are out in the mountains, please post your observations to the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A skier triggered size 1.5 avalanche was reported Monday on a north facing feature around 1700m. The crown was 30 to 50cm in depth and likely ran on the mid-November crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday natural storm slab avalanches to size 2 were reported on East, North, and Northwest facing features between 1900 and 2100m. These were likely running on the early December surface hoar. On Sunday control work in the region produced numerous avalanches to size 2 on SW, S and SE facing aspects between 1900 and 2000m. Late Sunday we received a report from the Rossland range where a group of skiers triggered a size 2.5 avalanche on a north facing piece of terrain at 1700m. The avalanche initially failed at the Mid-November crust before stepping down to the ground. Thankfully, it sounds like everyone involved will be okay.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Steady snowfall, high winds and rising freezing levels will make for dangerous avalanche conditions today. Size 1-2 soft slab avalanches have been observed over the last few days. Most have been running within the storm snow layers but a few isolated slabs have failed on the November 18th crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new was observed but visibility was very limited.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There have been reports of a widespread natural avalanche activity from the Whistler area that is likely indicative of what is going on in the rest of the Sea to Sky region. This cycle is expected to continue as a series of storms pummels the coast range over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">A widespread avalanche cycle is expected to continue as a series of storms pummels the coast range over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">It sounds like there were touchy conditions out there over the weekend. Reports of some large skier triggered and skier controlled avalanches from tree-line suggest that the load on the recently buried surface hoar is reaching critical levels.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday morning include widespread whumpfing, natural and remotely triggered Size 2 slab avalanches up to 50 cm deep. Explosives control produced 30-50cm deep slab avalanches up to Size 3.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Monday are limited, but include an isolated explosive-triggered Size 1 wind slab avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent reports of natural, rider and remotely triggered large slab avalanches from the mountains around Shames suggest that the load on a layer of recently buried surface hoar has reached critical levels.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday natural storm slab avalanches to size 2 were reported on East, North, and Northwest facing features between 1900 and 2100m. These were likely running on the early December surface hoar. On Sunday control work in the region produced numerous avalanches to size 2 on SW, S and SE facing aspects between 1900 and 2000m. Late Sunday we received a report from the Rossland range where a group of skiers triggered a size 2.5 avalanche on a north facing piece of terrain at 1700m. The avalanche initially failed at the Mid-November crust before stepping down to the ground. Thankfully, it sounds like everyone involved will be okay.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a natural cycle up to size 3 was reported from the deep snowpack area in the west of the region.  In the Selkirks to the west, three remotely triggered avalanches were reported, the furthest being triggered from 150m away. This suggests that the storm slab has gained enough cohesion for wide propagations. A widespread natural is expected to have occurred on Tuesday but there was no information at the time of publishing.  Touchy storms slab will continue to be sensitive to human-triggering at all elevations on Wednesday, especially at higher elevations where the snow remains dry. Remote-triggering may still be a concern, especially below 1800m where the surface hoar layer is most reactive. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, skiers triggered several storm slab avalanches up to size 1.5.  Two of these were remotely triggered from 15m away.  This suggests that the storm slab has gained enough cohesion for wide propagations. These released on the Dec 2 interface down 80-100cm.  A widespread natural cycle is expected to have occurred on Tuesday but there was no information at the time of publishing. Touchy storms slab will continue to be sensitive to human-triggering at all elevations on Wednesday, especially at higher elevations where the snow remains dry. Remote-triggering may still be a concern, especially below 1800m where the surface hoar layer is most reactive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday and Monday, several natural and human-triggered avalanches were reported up to size 3. These storm slabs were typically 50-90cm thick and occurred on all aspects and elevation bands. Of particular concern were a couple remotely triggered avalanches, the furthest being triggered from 40m away. This suggests that the storm slab is gaining cohesion and the propagation potential of the underlying weak layer is increasing. A widespread natural cycle is expected to have occurred on Tuesday but there was no information at the time of publishing.  Touchy storms slab will continue to be sensitive to human-triggering at all elevations on Wednesday, especially at higher elevations where the snow remains dry. Remote-triggering may still be a concern, especially below 1800m where the surface hoar layer is most reactive.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday and Monday, several natural and human-triggered avalanches were reported up to size 2.5. These storm slabs were typically 50-80cm thick and occurred on all aspects and elevation bands. Of particular concern were three remotely triggered avalanches, the furthest being triggered from 150m away. This suggests that the storm slab is gaining cohesion and the propagation potential of the underlying weak layer is increasing. A widespread natural cycle is expected to have occurred on Tuesday but there was no information at the time of publishing. Touchy storms slab will continue to be sensitive to human-triggering at all elevations on Wednesday, especially at higher elevations where the snow remains dry. Remote-triggering may still be a concern, especially below 1800m where the surface hoar layer is most reactive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread natural storm slab avalanches to size 2 were observed late yesterday above 1800m. Snowballing and loose wet avalanches were observed below tree line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several small loose dry avalanches were observed today mostly in steep Alpine terrain. Observation were somewhat limited due to limited visibility.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There have been reports of a widespread avalanche activity from the Whistler area that is likely indicative of what is going on in the rest of the Sea to Sky region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Monday, and Tuesday several natural and human-triggered storm slab avalanches were reported up to size 2.5. These storm slabs were typically 30-60cm thick and occurred on all aspects and elevation bands. Also reported were two very large wet slab avalanches but details were limited, likely due to visibility. Storm slabs are expected to remain sensitive to human-triggering on Thursday but natural activity should taper off now that the storm has ended. The exception might be steep sun-exposed slopes if the sun makes a longer appearance than expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">A widespread avalanche cycle is being reported as a series of storms pummels the coast range.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Tuesday and Wednesday morning include numerous explosive triggered storm slab avalanches and natural loose wet avalanches up to Size 2. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday morning include an overnight natural avalanche cycle with widespread avalanches up to Size 3.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">It sounds like there were touchy conditions out there over the weekend. Reports of some large skier triggered and skier controlled avalanches from tree-line suggest that the load on the recently buried surface hoar is probably at a critical level.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Monday, a natural cycle up to size 3 was reported from the deep snowpack area in the west of the region. On Tuesday, several natural size 2.5 were reported from higher elevations but details were limited due to visibility. Below treeline, ski-cutting produced several size 1 slabs from steep pockets of snow. These slabs were typically 15-30cm deep which suggests storm instabilities and not the deeper Dec 2 interface. Storm slabs are expected to remain sensitive to human-triggering on Thursday but natural activity should taper off now that the storm has ended. The exception might be steep sun-exposed slopes if the sun makes a longer appearance than expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Monday are limited, but include an isolated explosive-triggered Size 1 wind slab avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Widespread avalanche activity was reported throughout the recent storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Monday, skiers triggered several storm slab avalanches up to size 1.5. Two of these were remotely triggered from 15m away.&nbsp; These released on the Dec 2 interface down 80-100cm. Storm slabs are expected to remain sensitive to human-triggering on Thursday but natural activity should taper off now that the storm has ended. The exception might be steep sun-exposed slopes if the sun makes a longer appearance than expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Monday and Tuesday, several natural and human-triggered storm slab avalanches were reported up to size 2.5. These storm slabs were typically 30-50cm thick but one was 90cm thick. These occurred on all aspects and elevation bands. Also reported were two very large wet slab avalanches but details were limited, likely due to visibility. Storm slabs are expected to remain sensitive to human-triggering on Thursday but natural activity should taper off now that the storm has ended. The exception might be steep sun-exposed slopes if the sun makes a longer appearance than expected.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Natural avalanche activity diminished as freezing levels fell with the passage of the storm on Tuesday afternoon. Explosive testing and ski cutting yesterday was producing predominantly size 1.0 to 1.5 results within the storm snow layers, with a few to size 2.0. Strong winds from the south westerly direction yesterday. There were limited observations from outside the ski area yesterday due to poor weather conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">We’re continuing to receive reports of large storm slab avalanches from the Whistler area that is likely indicative of what is going on in much of the Sea to Sky region. This cycle is expected to continue as a series of storms pummels the coast range over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several naturally triggered storm slabs have occurred in the past 48hrs on N, NE and E aspects generally between 2700m and 2100m. These slides averaged 50cm in depth and ranged from size 1.5 to 2.5.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Natural avalanche activity is expected to slow as conditions continue to dry out and cool off over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday include numerous natural and skier-controlled 20-90cm thick storm slab avalanches up to Size 2 primarily on east through northeast aspects as low as 1600 m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday are limited but include evidence of a large natural avalanche cycle at alpine and treeline elevations with fresh debris visible in many paths and roaring avalanche heard throughout the day. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include evidence of the natural avalanche cycle Tuesday night into Wednesday morning, when heavy loading from snow, wind and rain produced slab and loose snow avalanches up to Size 3. With most slabs failing on the early December crust. Explosives control on Thursday produced 20-150cm thick slab avalanches up to Size 3.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Widespread avalanche activity was reported throughout the recent storm, with many of these avalanche reported to be releasing on a layer of surface hoar now buried between 70cm and 1m deep</span><span class="s_1681A555" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Monday, Tuesday &amp; Wednesday several natural and human-triggered storm slab avalanches were reported up to size 2.5. These storm slabs were typically 30-60cm thick and occurred on all aspects and elevation bands. A few spooky remotely triggered avalanches to size 2 were reported around 1500m too. Storm slabs are expected to remain sensitive to human-triggering on Friday, but natural activity should taper off now that the storm has ended. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Wednesday natural avalanches ran to size 3 on various aspects. Riders triggered avalanches to size 1.5 on N and NE facing features between 1600 and 2000m. Interesting to note that one rider triggered size 1.5 avalanche was actually remote triggered from 100m away on a steep north facing slope in a cutblock. The resulting avalanche had a 50cm deep crown. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">The layer of buried surface hoar is my biggest concern.  It is probably widespread and is reaching a burial depth that was associated with a rash of skier and remotely triggered avalanches in the deeper snowpack around Terrace last weekend.</span><span class="s_1681A555" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Monday and Tuesday, several natural and human-triggered storm slab avalanches were reported up to size 2.5. These storm slabs were typically 30-50cm thick but one was 90cm thick. These occurred on all aspects and elevation bands. Also reported were two very large wet slab avalanches but details were limited, likely due to visibility. On Wednesday natural avalanche activity did not exceed size 1.5. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations have been limited during the storm, especially from alpine elevations. On Monday, skiers triggered several storm slab avalanches up to size 1.5. Two of these were remotely triggered from 15m away, failing on the Dec 2 interface down 80-100cm. A large natural avalanche (size 2.5) was observed on a NE facing feature at 2000m Thursday. Observations from the Cariboos are limited right now and I suspect that recent avalanche activity is more widespread than the current data set would lead us to believe.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The widespread natural avalanche activity that occurred with rising freezing levels on Tuesday diminished as freezing levels fell with the passage of the storm on Tuesday afternoon. Periodical explosive testing and ski cutting since then was producing predominantly size 1.0 to 1.5 results within the storm snow layers, with a few to size 2.0. There have been limited observations from outside the ski area yesterday over the past several days due to poor weather conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new from the last 24hrs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include a remotely triggered Size 1.5 slab avalanche from a snowmobiler on a sheltered north facing slope below treeline that ran on surface hoar buried early-December. Other reports included more evidence of a large natural avalanche cycle at alpine and treeline elevations on Tuesday and Wednesday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include evidence of the natural avalanche cycle Tuesday night into Wednesday morning, when heavy loading from snow, wind and rain produced slab and loose snow avalanches up to Size 3. With most slabs failing on the early December crust. Explosives control on Thursday produced 20-150cm thick slab avalanches up to Size 3, with deeper slabs stepping down to the mid-November crust.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include an explosives-triggered 50cm thick persistent slab avalanche running on the early-December surface hoar on a convex roll below treeline in the Monashees.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Explosive avalanche control continues to produce slab avalanches on instabilities within the storm snow. Wind loaded pockets sitting above the rain crust have the most potential to be reactive to skier triggering.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Natural avalanche activity has slowed down although explosive tests suggest that human triggering may still be possible especially in wind loaded features in the alpine and at tree-line.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Widespread avalanche activity was reported through recent storm, with several avalanche releasing on the layer of surface hoar now buried between 70cm and 1m deep. Natural activity on this layer has slowed since the storm ended on Thursday. Explosive avalanche control around Shames produced smaller storm slab avalanches that released on mid-storm instabilities under larger triggers.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There is very little data coming from the region so this is largely conjecture. The layer of buried surface hoar is my biggest concern moving into the weekend. Where it exists it is probably reaching a burial depth of around 60cm. This depth was associated with several skier and remotely triggered avalanches in the deeper snowpack around Terrace last weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent observations have been very limited, but I suspect that recent avalanche activity is far more widespread than the current data set would lead us to believe. On Thursday a large natural avalanche (size 2.5) was observed on a NE facing feature at 2000m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A large natural avalanche cycle occurred on Thursday with several large natural avalanches to size 3 being reported on all aspects between 1300 and 2400m.  A few smaller rider triggered avalanches were also reported in various drainages on NE facing slopes.  One of the most interesting observations was of numerous avalanches to size 2.5 running on all aspects between 1400 and 1600m north of Revelstoke. These were likely running on the early December surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent observations have been very limited, but I suspect that recent avalanche activity is far more widespread than the current data set would lead us to believe. On Thursday a very large natural avalanche was observed on a SE facing feature at 2000m that initially failed below ridge crest and ran full path. In the neighboring North Columbia's Thursday was a very active day with the following activity being reported: &quot;A large natural avalanche cycle occurred on Thursday with several large natural avalanches to size 3 being reported on all aspects between 1300 and 2400m. A few smaller rider triggered avalanches were also reported in various drainages on NE facing slopes. One of the most interesting observations was of numerous avalanches to size 2.5 running on all aspects between 1400 and 1600m north of Revelstoke. These were likely running on the early December surface hoar.&quot;</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Control work in the central and southern Purcells Thursday produced avalanches to size 3.5 on a variety of aspects, some of which ran full path. On Friday a skier accidently triggered a size 2.5 avalanche on an east facing feature at 1500m in the northern Purcells. This avalanche failed on the early December Persistent Weak Layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosive and ski testing carried out within the ski area boundary yesterday produced numerous soft slabs to size 1.5.  The slabs were running within the storm snow layers and on the most recent crust.  The &quot;slack country&quot; received heavy traffic and little activity was observed.  Cornices have grown and they are moving easily.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new activity was observed on Saturday but there is evidence of some larger avalanches up to sz 2.5 that ran close to full path likely failing within the storm snow down 60cm.  See </span><a id='GoToAdded' href="http://www.facebook.com/kcpublicsafety" target="_blank"><span class="s_9255B882">facebook</span></a><span class="s_AA239A9B"> page for pictures. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include a remotely triggered Size 1.5 slab avalanche from a snowmobiler on a sheltered north facing slope below treeline that ran on surface hoar buried early-December. On Friday, ski cutting produced size 1 soft slabs in immediate lee features (generally north through east aspects).</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Thursday produced storm slab avalanches up to Size 3.&nbsp; These slabs were 20-150cm thick with the deeper slabs stepping down to the mid-November crust.&nbsp; On Friday, explosives triggered numerous storm slab avalanches up to size 2.&nbsp; These were 15-30cm thick soft slabs primarily on north through east aspects.&nbsp; This suggests that the wind loaded aspects are most likely to be reactive to human-triggering.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include an explosives-triggered 50cm thick persistent slab avalanche running on the early-December surface hoar on a convex roll below treeline in the Monashees.&nbsp; No new avalanches were reported on Friday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche observations have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday avalanche observations were limited to small cornice fall avalanches triggered by control work. Recent observations have been very limited, but I suspect that avalanche activity has been more widespread than the current data set would lead us to believe. On Thursday a very large natural avalanche was observed on a SE facing feature at 2000m that initially failed below ridge crest and ran full path. In the neighboring North Columbia's Thursday was a very active day with the following activity being reported: &quot;A large natural avalanche cycle occurred on Thursday with several large natural avalanches to size 3 being reported on all aspects between 1300 and 2400m. A few smaller rider triggered avalanches were also reported in various drainages on NE facing slopes. One of the most interesting observations was of numerous avalanches to size 2.5 running on all aspects between 1400 and 1600m north of Revelstoke. These were likely running on the early December surface hoar.&quot;</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday two significant observations were reported: The first was a size 3.5 natural avalanche that was observed on a SE facing feature at 2800m running to ground in some places. The second was a report of a skier triggered size 2.5 avalanche that was accidentally triggered on an east facing feature at 1500m in the northern Purcells. This avalanche failed on the early December Persistent Weak Layer. Control work in the central and southern Purcells Thursday produced avalanches to size 3.5 on a variety of aspects, some of which ran full path. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported from the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent observations have been very limited, but I suspect that recent avalanche activity is far more widespread than the current data set would lead us to believe. The last significant observation was from Thursday when a large natural avalanche (size 2.5) was observed on a NE facing feature at 2000m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">In recent days, explosives avalanche control in the north of the region produced a few wind slab avalanches to size 2. No other avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reported avalanche activity Friday was limited to control work induced storm slabs to size 1.5 on a north facing feature near treeline. On Thursday a large natural avalanche cycle occurred with several large natural avalanches to size 3 being reported on all aspects between 1300 and 2400m. A few smaller rider triggered avalanches were also reported in various drainages on NE facing slopes. One of the most interesting observations was of numerous avalanches to size 2.5 running on all aspects between 1400 and 1600m north of Revelstoke. These were likely running on the early December surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">I would expect a healthy round of storm slab activity in response to new snow and wind forecast for Saturday and Sunday. The timing of the natural avalanche activity is tough to pin-down, although weather models suggest touchiest conditions will develop around midnight on Saturday. Even though the storm is expected to taper-off on Sunday, I would have serious concerns for ongoing human triggering of large new storm slabs, especially in higher-elevation, wind-exposed terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">I expect a healthy round of storm slab activity in response to new snow and wind forecast for Saturday and Sunday. The timing of the natural avalanche activity is tough to pin-down, although weather models suggest touchiest conditions will develop around midnight on Saturday. Even though the storm is expected to taper-off on Sunday, I would have serious concerns for ongoing human triggering of new storm slabs, especially in higher-elevation, wind-exposed terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We observed little in the way of avalanche activity yesterday. There has already been some loose sluffing this morning and you can expect to see soft slab activity in the alpine and at treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new observed or reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new natural avalanches have been reported since Wednesday. On Saturday, explosives triggered storm slabs up to size 2. These slabs were 5-15cm thick and were running on the thick melt-freeze crust. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday and Saturday, explosives produced storm slabs up to size 2.  These were typically 15-30cm thick soft slabs primarily on north through south-east aspects. One of these explosive triggered avalanches on Saturday stepped down to the mid-Nov crust/facet layer down 70cm on a SE aspect.  On Sunday, explosives triggered one size 2 avalanche which also failed on the mid-Nov crust/facet layer.  This was on a steep SE aspect at 1700m elevation and the slab was 30-100cm thick.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No avalanches were reported on Saturday or Sunday. This likely speaks to a lack of observations rather than actual conditions. I'm sure there was a round of natural storm slab activity in response to new snow and wind on Saturday. If you have any observations to share, please consider trying our Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">At the time of publishing, there was little information available regarding avalanche activity in the region. However, there were some reports of explosive controlled storm slabs to size 2.5 in lee alpine features. In at least one case, the avalanche failed on a rain crust approximately 100cm below the surface.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, ski cutting produced size 1 soft slabs in immediate lee features (generally north through east aspects). On Saturday, explosives and ski cutting produced storm slabs size 1-2 which were typically 20-60cm thick. On Sunday, explosives triggered a few size 2 wind slabs which were typically 30cm thick.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported from the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, ski cutting produced a size 1.5 wind slab avalanche. This occurred in a steep, open, wind-loaded feature and the slab was 15-50cm thick. The bed surface was the rain crust from last week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No avalanche activity to report from Saturday. On Friday two significant observations were reported: The first was a size 3.5 natural avalanche that was observed on a SE facing feature at 2800m running to ground in some places. The second was a report of a skier triggered size 2.5 avalanche that was accidentally triggered on an east facing feature at 1500m in the northern Purcells. This avalanche failed on the early December Persistent Weak Layer. Control work in the central and southern Purcells Thursday produced avalanches to size 3.5 on a variety of aspects, some of which ran full path. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Large natural sluffs to size 1.5 were reported from all aspects between 1300m and 2400m Saturday. The last significant observation was from Thursday when a large natural avalanche (size 2.5) was observed on a NE facing feature at 2000m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report from Saturday. On Friday reported avalanche activity was limited to control work induced storm slabs to size 1.5 on a north facing feature near treeline. On Thursday a large natural avalanche cycle occurred with several large natural avalanches to size 3 being reported on all aspects between 1300 and 2400m. A few smaller rider triggered avalanches were also reported in various drainages on NE facing slopes. One of the most interesting observations was of numerous avalanches to size 2.5 running on all aspects between 1400 and 1600m north of Revelstoke. These were likely running on the early December surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new activity to report from Saturday. On Friday avalanche observations were limited to small cornice fall avalanches triggered by control work. On Thursday a very large natural avalanche was observed on a SE facing feature at 2000m that initially failed below ridge crest and ran full path. In the neighboring North Columbia's Thursday was a very active day with the following activity being reported: &quot;A large natural avalanche cycle occurred on Thursday with several large natural avalanches to size 3 being reported on all aspects between 1300 and 2400m. A few smaller rider triggered avalanches were also reported in various drainages on NE facing slopes. One of the most interesting observations was of numerous avalanches to size 2.5 running on all aspects between 1400 and 1600m north of Revelstoke. These were likely running on the early December surface hoar.&quot;</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There were several size 1-2 slab avalanches yesterday with explosive and ski testing. There was also evidence of a mid storm natural cycle.</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">Isolated naturally triggered sluffs up to size 1.0 were observed today in steep Alpine terrain on N, NE and E aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">During the storm on Saturday, slab avalanches could be readily triggered by skiers. However, ski-cutting on Monday produced no results.</span></p>
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</style><p class="p_CC664AAA"><span class="s_CDCF4B37">Avalanche activity appears to have tapered off since Friday. Reports from over the weekend describe mainly small explosively controlled avalanches in steep terrain. The exception was a small skier triggered avalanche that ran on the December 2</span><sup><span class="s_CDCF4B37">nd</span></sup><span class="s_CDCF4B37"> surface hoar near in the Panorama slack country. On Friday two significant observations were reported: The first was a natural size 3.5 avalanche that was observed on a SE facing feature at 2800m in the Bugaboos. It ran to ground in some places. The second was a report of a skier triggered size 2.5 avalanche in the DogTooth range that was accidentally triggered on an east facing feature at 1500m. This avalanche failed on the early December Persistent Weak Layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since Friday. Reports from over the weekend describe sluffs in steep terrain, natural avalanches up to size 1.5 failing on a mid-storm instability, and skier and explosive controlled avalanches in steep or wind loaded features. No new avalanches were reported to have released on the layer of buried surface hoar over the weekend,</span><span class="s_1681A555"> </span><span class="s_AD4A7DB8">although this may be because people have been avoiding locations where it likely to be found. Because the consequences of triggering this layer could be catastrophic I'm keeping it in mind for the time being.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">Avalanche activity appears to have tapered off since Friday. Reports from the Columbia Mountains over the weekend detail sluffs in steep terrain, natural slab avalanche up to size 2 failing on a mid-storm instability, and skier controlled avalanche on wind loaded features</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a skier was caught in a size 1.5 avalanche on a northeast aspect at 1900 m. Explosive avalanche control was able to produce size 2 avalanches in the recent storm snow. Previously, an explosive triggered avalanche on Saturday stepped down to the nid-Nov crust/facet layer down 70 cm on a southeast aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a couple of size 2 avalanches were reportedly triggered by skiers in steep north and northeast facing slopes. Over the weekend, explosives and ski cutting produced storm slabs size 1-2 which were typically 20-60cm thick.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since Friday. Reports from over the weekend describe sluffs in steep terrain, natural avalanches up to size 2 failing on a mid-storm instability, and skier controlled avalanches in steep or wind loaded features. No new avalanches were reported to have released on the layer of buried surface hoar over the weekend,</span><span class="s_1681A555"> </span><span class="s_AD4A7DB8">although this may be because people have been avoiding locations where it likely to be found.. Because the consequences of triggering this layer could be catastrophic Im keeping it in mind for the time being.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend, size 1 and size 2 avalanches could be triggered by skiers and explosive avalanche testing in the newly deposited storm snow on north aspects between 1900 and 2100 m. I anticipate avalanches will become harder to trigger as the storm snow settles and temperatures drop.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There have been no recent reports of avalanche activity. This may speak more to a lack of observations rather than actual conditions. If you've been out in the mountains, please share your observations on the Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Explosives testing on Sunday produced storm slabs to size 2.5 in high elevation lee terrain. Most of the observed avalanche activity released within the new storm snow.; however, in at least 2 cases slabs released on a buried crust. At the time of publishing, no new avalanches were observed on Monday.</span></p><p class="p_CC664AAA"><span class="s_A8FEC758"> </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">In recent days small pockets of wind slab were observed failing naturally with minimal propagation in the lee of alpine ridge crests. Wind and snow forecast for Monday night and Tuesday will likely spark a new round of wind slab activity in the alpine and at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported from the region. With new wind and snow forecast for Monday night, I would expect a new round of wind slab activity at treeline and in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 1 soft slabs with explosive testing in the morning and solar point releases with sun warming in the afternoon yesterday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new from the last 24hours.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a couple of size 2 avalanches were reportedly triggered by skiers in steep north and northeast facing slopes. Over the weekend, explosives and ski cutting produced storm slabs size 1-2 which were typically 20-60cm thick.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. On Monday, a skier was caught in a size 1.5 avalanche on a northeast aspect at 1900 m. Explosive avalanche control was able to produce size 2 avalanches in the recent storm snow. Previously, an explosive triggered avalanche on Saturday stepped down to the mid-Nov crust/facet layer down 70 cm on a southeast aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend, size 1 and size 2 avalanches could be triggered by skiers and explosive avalanche testing in the newly deposited storm snow on north aspects between 1900 and 2100 m. I anticipate avalanches will become harder to trigger as the storm snow settles and temperatures drop.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Some wind slabs near ridgetops may continue to be triggered by light additional loads. Thin new wind slabs may develop over night due to forecast new snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported from the region. This may speak more to a lack of observations rather than actual conditions. I would expect newly formed wind slabs to be sensitive to human triggering for the next few days in high elevation lee terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">At the time of publishing this bulletin, there were no new reports of avalanche activity. I'm sure there was a round of new wind slab activity on Tuesday in response to new snow and strong winds. New wind slabs may remain sensitive to human triggering for longer than normal due to the presence of underlying surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend. Avalanche professionals in the field are reporting sluffing in steep terrain in response to skier traffic (aka good riding conditions) and some lingering reactive pockets of wind slab in steep lee features. No new avalanches have been reported on the layer of buried surface hoar since last week,</span><span class="s_1681A555"> however, people have been experiencing </span><span class="s_AD4A7DB8">wumphing and other signs of instability from safe terrain as they travel between 1400 and 1800m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend.  Avalanche professionals in the field are reporting sluffing in steep terrain in response to skier traffic (aka good skiing). No new avalanches have been reported on the layer of buried surface hoar since last week,</span><span class="s_1681A555"> </span><span class="s_AD4A7DB8">although this may be because people have been avoiding locations where it is likely to be found.</span><span class="s_CDCF4B37" /></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend. Avalanche professionals in the field are reporting sluffing in steep terrain in response to skier traffic (aka good skiing). No new avalanches have been reported on the layer of buried surface hoar since last week,</span><span class="s_1681A555"> </span><span class="s_AD4A7DB8">although this may be because people have been avoiding locations where it is likely to be found.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend. Avalanche professionals are reporting sluffing in steep terrain and in response to ski cutting. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Monday there were a few reports of small loose wet avalanches running on steep, sun-exposed slopes. They occurred in response to solar radiation and brief warming. On Tuesday, we received reports of human-triggered wind slab activity to size 1 on exposed convex rolls at treeline and in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">A MIN report from Mt Rohr (Duffey Lake area) indicated a size 3 slab avalanche in unsupported alpine terrain which likely failed during the storm on the weekend. No other recent avalanche activity was noted. If you've been out in the mountains, we'd love to hear from you. Please share your observations on our Mountain Information Network.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. I suspect that pockets of wind slab may continue to be triggered by light additional loads in the alpine and at treeline. New storm slabs are expected to develop with the incoming storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little to no avalanche activity this past week either naturally, explosive or human triggered.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend.  Avalanche professionals in the field are reporting sluffing in steep terrain in response to skier traffic (aka good riding conditions) and some lingering reactive pockets of wind slab in steep lee features. No new avalanches have been reported on the layer of buried surface hoar since last week,</span><span class="s_1681A555"> however, people have been experiencing </span><span class="s_AD4A7DB8">wumphing and other signs of instability from safe terrain as they travel between 1400 and 1800m.</span><span class="s_AD4A7DB8" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported from the region. This may speak more to a lack of observations rather than actual conditions. I would expect newly formed wind slabs to be sensitive to human triggering for the next few days in high elevation lee terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new natural avalanches reported. Some explosive controlled cornice was reported up to size 2.0 on Tuesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new natural avalanches reported.</span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend. Avalanche professionals in the field are reporting sluffing in steep terrain in response to skier traffic (aka good skiing). No new avalanches have been reported on the layer of buried surface hoar since last week,</span><span class="s_1681A555"> </span><span class="s_AD4A7DB8">although this may be because people have been avoiding locations where it is likely to be found.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend. Avalanche professionals in the field are reporting sluffing in steep terrain in response to skier traffic (aka good skiing). No new avalanches have been reported on the layer of buried surface hoar since last week,</span><span class="s_1681A555"> </span><span class="s_AD4A7DB8">although this may be because people have been avoiding locations where it is likely to be found.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">Avalanche activity appears to have tapered off since the weekend. Avalanche professionals are reporting sluffing in steep terrain and in response to ski cutting.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Thin new wind slabs may develop in response to new snow and wind in exposed areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a skier near Fernie was caught in a size 2 avalanche on an east aspect that appeared to be triggered in wind slab at an exposed location. The avalanche was 20-30 cm deep, around 50 m wide and about 500 m long. More details</span><a id='GoToAdded' href="http://www.avalanche.ca/share/auto-quick-report/59c4b8d9-cc71-48c8-ba44-f01e058180aa" target="_blank"><span class="s_B5813F7D"> are here</span></a><span class="s_3FE45715">: http://bit.ly/228sRCl. On Monday, a skier was caught in a size 1.5 avalanche on a northeast aspect at 1900 m. Explosive avalanche control was able to produce size 2 avalanches in the recent storm snow. Previously, an explosive triggered avalanche on Saturday stepped down to the mid-Nov crust/facet layer down 70 cm on a southeast aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a couple of size 2 avalanches were reportedly triggered by skiers in steep north and northeast facing slopes. Over the weekend, explosives and ski cutting produced storm slabs size 1-2 which were typically 20-60cm thick.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Only sluffing of the new snow in steep terrain has been reported since the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Small size one slabs avalanches may be triggered from steep start zones in isolated areas. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing to speak of, however field observations were limited today.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Incremental loading should develop thin new wind slabs on lee aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Widespread new storm slabs are expected to develop with the forecast snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new natural avalanches reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A few loose dry avalanches up ti size 1.5 were reported from Wednesday. Expect widespread storm slabs to develop with forecast new snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">One size 2.0 natural wind slab was reported from Wednesday east of Terrace in the Skeena valley at about 1400 metres. New storm slabs are expected to develop with the incoming storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">Ski cuts have been able to produce size small wind slab avalanche in alpine lee features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche professionals in the field are reporting small slab avalanches in the immediate lee of wind loaded features.</span><span class="s_AD4A7DB8" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a skier near Fernie was caught in a size 2 avalanche on an east aspect that appeared to be triggered in wind slab at an exposed location. The avalanche was 20-30 cm deep, around 50 m wide and about 500 m long. More details</span><a id='GoToAdded' href="http://www.avalanche.ca/share/auto-quick-report/59c4b8d9-cc71-48c8-ba44-f01e058180aa" target="_blank"><span class="s_B5813F7D"> are here</span></a><span class="s_3FE45715">: http://bit.ly/228sRCl. On Monday, a skier was caught in a size 1.5 avalanche on a northeast aspect at 1900 m. While there have been no further reports of avalanche activity since the event on Tuesday, I anticipate the chance of natural and human-triggered avalanches will increase during Friday's storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a couple of size 2 avalanches were reportedly triggered by skiers in steep north and northeast facing slopes. Since then no further avalanches have been noted in this region. I anticipate the chance of both natural and human triggered avalanches will increase during the expected storm on Friday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">There have been no reports of recent avalanche activity.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche activity appears to have tapered off since the weekend. Avalanche professionals in the field are reporting sluffing in steep terrain in response to skier traffic (aka good skiing). No new avalanches have been reported on the layer of buried surface hoar since last week,</span><span class="s_1681A555"> </span><span class="s_AD4A7DB8">although this may be because people have been avoiding locations where it is likely to be found.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche professionals in the field are reporting small slab avalanches in the immediate lee of wind loaded features.</span><span class="s_AD4A7DB8" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The new storm snow is likely to be triggered as storm slabs in the alpine. The new snow is releasing as small size one soft storm snow slabs at and below tree-line.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche professionals in the field are reporting sluffing in extreme terrain, and small soft slabs in the immediate lee of wind loaded features are reactive to skier traffic.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche professionals in the field are reporting small slab avalanches in the immediate lee of wind loaded features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche professionals in the field were reporting sluffing in extreme terrain and isolated pockets of reactive wind slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AD4A7DB8">Avalanche professionals in the field are reporting sluffing in extreme terrain, and small soft slabs in the immediate lee of wind loaded features are reactive to skier traffic.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Lots of sluffing on the steep faces today. The sluffing has created small slabs at the base of cliffs. In a few cases, these slabs did release. The biggest was a sz1, on a steep East aspect at 2200m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Extensive wind effect reported in the alpine and at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Incremental loading should develop thin new wind slabs on lee aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Suspect widespread thin soft slabs were easy to trigger today due tot the dry snow and moderate winds.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread loose dry activity up to size 1.5 and explosives control up to size 2.0 has been reported from Whistler Friday morning. I suspect that some pockets of wind transported snow may be easy to trigger on lee aspects. Watch for longer fracture propagations resulting in larger avalanches as the new storm snow load increases and settles into a cohesive slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Widespread new storm slabs are expected to continue to develop with the forecast snow and wind this weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_7D940460">No new avalanches to report from Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Control work on Friday produced 5 to 10cm thick wind slabs that ran as large as size 1.5 in isolated terrain features. No other activity to report.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday control work in the Lizard Range produced storms slabs to size 1 on a SE facing feature at 2000m. On Tuesday, a skier near Fernie was caught in a size 2 avalanche on an east aspect that appeared to be triggered in a wind slab at an exposed location. The avalanche was 20-30 cm deep, around 50 m wide and about 500 m long. More details</span><a id='GoToAdded' href="http://www.avalanche.ca/share/auto-quick-report/59c4b8d9-cc71-48c8-ba44-f01e058180aa" target="_blank"><span class="s_B5813F7D"> are here</span></a><span class="s_3FE45715">: http://bit.ly/228sRCl. On Monday, a skier was caught in a size 1.5 avalanche on a northeast aspect at 1900 m. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed today. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Soft windslabs released naturally or were triggered by fresh cornice falls in the Duffy Lake area on Friday up to size 2.0</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday we received observations of several small (size 1) avalanches on south facing aspects at treeline. Crown depths were no more than 15cm in depth which suggests that the new snow is bonding quickly to the old surface.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new natural avalanches reported. Skiers have reported easy to trigger pockets of windslab up to 100 cm deep that have been confined to steep un-supported features and have not run far.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Incremental loading should develop thin new wind slabs on lee aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Soft cornice noses are falling on their own, while size one to 1.5 storm slabs have been easily triggered over the past 36 hours.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Extensive wind effect reported in the alpine and at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Observations were limited on Saturday; however, an explosive-controlled size 2 wind slab was observed on a north-facing alpine slope. Continued strong winds and new snow will likely be the driver for continued wind slab avalanche activity over the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">Recently, natural and human-triggered wind slab avalanches in the size 1-1.5 range were observed in the alpine and at treeline. Continued strong winds and new snow will likely be the driver for continued wind slab avalanche activity over the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Recently, natural and human-triggered wind slab avalanches in the size 1-1.5 range were observed in the alpine and at treeline. Continued strong winds and new snow will likely be the driver for continued wind slab avalanche activity over the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There have been no recent reports of avalanche activity. This may speak more to a lack of observations rather than actual conditions. Wind and new snow will likely be the driver for wind slab avalanche activity over the next few days.</span><span class="s_AD4A7DB8" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Control work on Friday produced widespread 10 to 15cm thick wind slabs that ran as large as size 1.5 on a variety of aspects above 1800m. On Tuesday of last week, a skier near Fernie was caught in a size 2 avalanche on an east aspect that appeared to be a wind slab. The avalanche was 20-30 cm deep, around 50 m wide and about 500 m long. More details are here: http://bit.ly/228sRCl. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report from the South Rockies. In the neighboring Lizard Range, control work on Friday produced widespread 10 to 15cm thick wind slabs that ran as large as size 1.5 on a variety of aspects above 1800m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_7D940460">No new avalanches to report from Thursday or Friday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose dry avalanches up to size 1.0 were observed in extreme terrain in the Alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Skiers triggerd a thin ( 20 cm deep) storm slab on a poorly supported&nbsp; east aspect in the Coquihalla that suggests that wider fracture propagations are possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Soft new storm slabs releasing up to size 2.0 and new cornices releasing naturally to size 1.5 at Whistler.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Incremental loading should develop thin new wind slabs on lee aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A natural avalanche cycle was observed on Saturday night, with several size 1-2 storm slabs. Crowns were typically 50 cm deep. Skiing on Sunday also produced an avalanche and shooting cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several small naturals were reported from steep rock slabs at low elevations above the highway. No new avalanche reported from higher elevations. Suspect travel and visibility may have been restricted by stormy conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Observations were limited on Saturday and Sunday; however, an explosive-controlled size 2 wind slab was observed on a north-facing alpine slope. Continued strong winds and new snow from Sunday will likely be the driver for human-triggered wind slab avalanche activity over the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday, explosives produced several avalanches up to size 2 within the storm snow. There was a natural avalanche cycle on Saturday, with several size 1-2 storm slabs at alpine and treeline elevations. Explosives testing also produced several storm/wind slabs, the largest at size 2.5. On Tuesday of last week, a skier near Fernie was caught in a size 2 avalanche on an east aspect that appeared to be a wind slab. More details are here: http://bit.ly/228sRCl.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Skiers triggered size 1 loose dry avalanches on Saturday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">Recently, natural and human-triggered wind slab avalanches in the size 1-1.5 range were observed in the alpine and at treeline. As the stormy weather tapers-off, so should natural avalanche activity. However, wind slab avalanches may remain sensitive to human-triggering for a few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Saturday there was evidence of 2 size 1.5 natural persistent slab avalanches. They failed between 1000 and 1100m, ran for about 100m and were up to 80cm deep. The early December surface hoar interface was the likely culprit in these events  I'm sure there has also been a widespread round of natural wind slab activity in response to new snow and wind on Saturday night and Sunday. As the stormy weather eases, I'd expect natural wind slab activity to taper-off; however, human triggering will likely remain a real concern for a few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Recently, natural and human-triggered wind slab avalanches in the size 1-1.5 range were observed in the alpine and at treeline. While natural wind slab activity may taper-off as the weather eases, human triggering will likely remain a concern in higher elevation lee terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">One loose dry naturally triggered avalanche was observed today on a steep NW aspect initiating in the Alpine. This slide was a size 1.5 and ran for a significant distance.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Observations were limited on the weekend, although touchy wind slab avalanches to 20cm in depth were being triggered near ridgetop in response to new snow and wind in the north of the region. I'd anticipate the possibility of human-triggered wind slab avalanche activity over the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">Several small naturals were reported from steep rock slabs at low elevations above the highway. No new avalanche reported from higher elevations although I suspect that travel and visibility may have been restricted by stormy conditions.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Sunday, we received a few reports of widespread natural and human-triggered wind slab avalanche activity to size 2. As the weather eases, so should natural wind slab avalanche activity. That said, human triggering will remain a concern for a few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Wind slabs were reported to have developed at all elevations on Monday, but at the time of writing no avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">No new avalanches have been reported over the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Saturday there was evidence of 2 size 1.5 natural persistent slab avalanches. They failed between 1000 and 1100m, ran for about 100m and were up to 80cm deep. The early December surface hoar interface was the likely culprit in these events I'm sure there has also been a widespread round of natural wind slab activity in response to new snow and wind on Saturday night and Sunday. As the stormy weather eases, I'd expect natural wind slab activity to taper-off; however, human triggering will likely remain a concern for a few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A widespread natural avalanche cycle ran on Saturday night/ Sunday, with several size 1-2 storm slabs. Crowns were typically 50 cm deep. Skiing on Sunday also produced avalanches and shooting cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Sunday, we received a few reports of widespread natural and human-triggered wind slab avalanche activity to size 2. As the weather eases, so should natural wind slab avalanche activity. That said, human triggering will remain a concern for a few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">Explosive avalanche control produced storm slab avalanches up to size 2 over the weekend. These mainly ran on mid storm instabilities although some failed on the old snow surface now down 50-70cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Skiers triggered numerous loose dry and soft slab avalanches on Sunday in the size 1-2 range. There were also numerous natural loose dry and storm slab avalanches out of steep terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Sunday and Monday, explosives produced several avalanches up to size 2 within the storm snow. There was a natural avalanche cycle on Saturday, with several size 1-2 storm slabs at alpine and treeline elevations. Explosives testing also produced several storm/wind slabs, the largest at size 2.5. By Monday morning, limited reports suggested the storm snow was starting to bond better. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There were reports of some large natural and explosive controlled storm slab avalanches north of Pemberton on Sunday.  People were also able to find reactive pockets of wind slab in the Coquihalla at upper elevations over the weekend</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Soft cornice noses are falling on their own, while size one to 1.5 storm slabs have been easily triggered over the past 36 hours.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some small loose dry avalanches from the last 48hrs are still visible. These are isolated to steep, gully features. A cornice collapse was also noted today from a distance. There didn't appear to be any propagation of the slope below. Sz 1.5, SE asp 2500m</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">Small loose avalanches have been reported in steep terrain in the alpine. There haven't been any reports of recent avalanche activity on any buried layers of surface hoar. However, I suspect that as the new snow continues to settle well start to see these layers wake up. It's difficult to predict when that will be with the slow incremental loading pattern we're dealing with</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Skiers triggered numerous loose dry and soft slab avalanches on Sunday in the size 1-2 range. There were also numerous natural loose dry and storm slab avalanches out of steep terrain. On Monday, skier triggering eased, but explosives still produced several size 1-2 storm slabs. </span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several storm slabs and loose dry avalanches in the size 1-2 range have been reported over the last few days. Most of these have been in the alpine and on lee slopes and spill zones. Loose dry sluff has also been running on steep slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A few naturally triggered size 1-2.5 storm slabs have been observed over the last two days. Numerous loose dry avalanches were also reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Avalanche activity appears to have tapered off since the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Evidence of a few natural wind slab avalanches to size 2 was observed in lee alpine terrain on Monday and Tuesday. The avalanches occurred in response to new snow and wind on the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Evidence of a natural cycle of soft wind slab avalanches in the size 1-2 range was observed on Monday. The avalanches occurred in response to new snow and wind over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">Avalanche activity appears to have tapered off since the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A widespread natural avalanche cycle ran on Saturday night/ Sunday, with several size 1-2 storm slabs. Crowns were typically 50 cm deep. Skiing on Sunday also produced avalanches and shooting cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Evidence of a fairly widespread cycle of soft wind slab avalanches in the size 1-1.5 range was observed in extreme terrain on Monday. The avalanches occurred in response to new snow and wind over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Evidence of a natural cycle of soft wind slab avalanches in the size 1-2 range was observed on Monday. The avalanches occurred in response to new snow and wind over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosive and ski testing carried out after last weekends storm produced numerous size 1-1.5 avalanches that were running within the storm snow and on the old hard surfaces. A few isolated size 2 results failed on the December 8th crust and the crown lines were up to 1.5 m. in depth. Cornices proved to be very touchy. A skier accidental size 1.5 avalanche was observed yesterday outside the ski area on Oboe at the treeline elevation. We suspect this ran on Monday. The crown line was 75 cm deep by 25m wide, and the failure plane was a layer of surface hoar that was buried on Dec 17th.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Explosive and ski testing carried out after last weekends storm produced numerous size 1-1.5 avalanches that were running within the storm snow and on the old hard surfaces. A few isolated size 2 results failed on the December 8th crust and the crown lines were up to 1.5 m. in depth. Cornices proved to be very touchy. A skier accidental size 1.5 avalanche was observed yesterday outside the ski area on Oboe at the treeline elevation. We suspect this ran on Monday. The crown line was 75 cm deep by 25m wide, and the failure plane was a layer of surface hoar that was buried on Dec 17th.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new was seen today</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">Avalanche activity appears to have tapered off since the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Evidence of a few natural wind slab avalanches to size 2 was observed in lee alpine terrain on Monday and Tuesday. The avalanches occurred in response to new snow and wind on the weekend. On Wednesday morning in the Golden backcountry, a size 2 skier-triggered wind slab avalanche occurred on a northwest aspect at about 2400m. It was up to 50cm in depth and ran approximately 600m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Avalanche activity appears to have tapered off.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">No new avalanche have been reported. The lack of recent avalanche activity the buried layers of surface hoar don't mean they are not a problem. I suspect that as the new snow continues to settle we could start to see these layers wake up although it's difficult to predict when that will be.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanche observations.&nbsp; A widespread natural avalanche cycle ran on Saturday night/ Sunday, with several size 1-2 storm slabs. Crowns were typically 50 cm deep. Skiing on Sunday also produced avalanches and shooting cracks.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday control work produced storm slab avalanches to size 2.5. On Sunday and Monday several storm slabs and loose dry avalanches to size 2 were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches to report from Tuesday. On Sunday and Monday a few naturally triggered size 1 to 2.5 storm slabs and numerous loose dry avalanches were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches to report from Tuesday. On Monday, skier triggering of avalanches eased, but control work still produced several size 1 to 2 storm slabs. On Sunday skiers triggered numerous loose dry and soft slab avalanches in the size 1 to 2 range. There were also numerous natural loose dry and storm slab avalanches out of steep terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 1 loose natural avalanche activity and point releases were observed this morning in steep terrain at tree line elevation. These new snow layers have very little in the way of destructive potential. Explosive and ski testing carried out on Monday produced numerous size 1-1.5 avalanches that were running within the storm snow and on the old hard surfaces. A few isolated size 2 results failed on the December 8th crust and the crown lines were up to 1.5 m. in depth. Cornices proved to be very touchy. A skier accidental size 1.5 avalanche was observed on tuesday outside the ski area on Oboe at the tree-line elevation that was suspected to have run on Monday. The crown line was 75 cm deep by 25m wide, and the failure plane was a layer of surface hoar that was buried on Dec 17th.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few loose dry slides out of steep unskiable terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, two natural size 2.5 glide crack releases were reported but no details were attached. Minor sluffing from steep terrain was also reported in the region. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent slab avalanches have been reported.  Minor sluffing from steep terrain was reported on Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported since Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A size 2 skier triggered avalanche was reported from the Joffre group on Wednesday. It released on a wind loaded feature at ridgeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">The most recent storm snow is sluffing in steep terrain with minimal destructive potential. Some larger storm slab avalanche have been reported from the North Shore where conditions may be closer to what can be found around Garibaldi. Further north, a skier was involved in a size 2 avalanche in the Joffre group on Wednesday that released from a wind loaded pocket at ridgeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">No recent avalanche have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Evidence of a few natural wind slab avalanches to size 2 was observed in lee alpine terrain on Monday and Tuesday. The avalanches occurred in response to new snow and wind on the weekend. On Wednesday, two skier accidental avalanches were reported in the Golden backcountry. The first occurred in the morning and was a size 2 wind slab avalanche which occurred on a northwest aspect at about 2400m. It was up to 50cm in depth and ran approximately 600m. The second occurred in the afternoon and was a size 2.5 wind slab at ridgetop. This also occurred on a NW aspect at 2400m elevation. The avalanche stepped down to a deeper layer lower down in the start zone, likely the early December interface.&nbsp; On Thursday, a large settlement was felt in a flat meadow in the Invermere backcountry.&nbsp; This occurred at 2200m in a below treeline terrain feature and the failure layer is unknown.</span></p>
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</style><p class="p_CC664AAA"><span class="s_69982360">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday the new new/old snow interface was quite touchy. We received multiple reports of remote triggering of small shallow storm slabs from as far away as 100m on all aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday one natural size 2 was observed in steep alpine terrain on an unknown aspect.&nbsp; Control work Wednesday produced storm slabs to size 2 on all aspects.&nbsp; Crown depths ranged from 10 to 60cm in depth with the bulk of the crowns in the 10 to 20cm range.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday we received a report of a skier triggered size 1 wind slab on a north aspect at 1800m. It's thought that this avalanche failed on the December 9th melt freeze crust which was down 40cm at the location of the avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent avalanche activity has been limited to small loose snow avalanches on steep features and small wind slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 1 loose natural point releases ran yesterday in steep terrain at tree line elevations. These new snow sluffs have little in the way of destructive potential. Cornices noses are very touchy. A skier accidental size 1.5 avalanche was observed on Tuesday outside the ski area on the backside of Oboe at about 1900m. It was likely 24 hr. old. The crown line was 75 cm deep by 25m wide, and the failure plane was a layer of surface hoar that was buried on December 17th.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There haven't been any reports of recent natural activity but people have been getting surprised by isolated pockets of wind slab. A skier was involved in a size 2 avalanche in the Joffre group on Wednesday that released from a wind loaded pocket at ridgeline.&nbsp; Another group of skiers were startled by a wind slab on a cross loaded feature at treeline in the Spearhead on Tuesday. Guides in the area are reporting that cornices are getting large and are them with caution.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">The most recent storm snow is sluffing in steep terrain with minimal destructive potential. There haven't been any recent reports of natural slab avalanche activity in the Sea to Sky but some avalanches in neighboring regions are worth keeping in mind. Storm slab activity was reported from the North Shore&nbsp; as recently as Thursday, where conditions may be closer to what can be found around Garibaldi. Further north, a skier was involved in a size 2 avalanche in the Joffre group on Wednesday that released from a wind loaded pocket at ridgeline. On Tuesday several skiers were surprised by a wind slab on a cross loaded feature at treeline in the Spearhead. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent slab avalanches have been reported. Minor sluffing from steep terrain was reported on Wednesday. On Thursday, explosives produced only loose sluffing from steep terrain features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">No new avalanche have been reported as publishing on Friday afternoon.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, two natural size 2.5 glide crack releases were reported but no details were attached. Four small natural wind slabs were also reported from steep NW aspects in the alpine.  Minor natural sluffing from steep terrain was also reported in the region on Wednesday. No natural avalanches were reported on Thursday and explosives only triggered loose sluffing from steep slopes on a variety of aspects.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">No recent avalanche have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, two skier accidental avalanches were reported in the Golden backcountry. The first occurred in the morning and was a size 2 wind slab avalanche which occurred on a northwest aspect at about 2400m. It was up to 50cm in depth and ran approximately 600m. The second occurred in the afternoon and was a size 2.5 wind slab at ridgetop. This also occurred on a NW aspect at 2400m elevation. This avalanche stepped down to a deeper layer lower down in the start zone, likely the early December interface. On Thursday, a large settlement was felt in a flat meadow in the Invermere backcountry. This occurred at 2200m in a below treeline terrain feature and the failure layer is unknown.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported since Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday a skier triggered an avalanche that partially buried two people in the party near 1st Pump Peak on Seymour. Details here: http://bit.ly/1MzDfHM&nbsp; Widespread touchy storm slabs released naturally Wednesday night with an average crown depth of 30cm. This comes on the heels of all the activity reported during the day on Wednesday when the new new/old snow interface was quite touchy.&nbsp; On Wednesday we received multiple reports of remote triggering of small shallow storm slabs from as far away as 100m on all aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent avalanche activity has been limited to fast running loose snow avalanches on steep features and small wind slabs in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Lot's of avalanche activity was reported Thursday with control work producing storm slabs up to size 1.5, with the bulk of the activity occurring on north and northeast facing slopes between 1500 and 2100m.  Intentional ski cutting produced avalanches to size 1 that ran in the new storm snow.  Control work triggered one large (size 2.5) avalanche that ran on the mid-December surface hoar on an unknown aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday control work produced numerous small loose snow avalanches within the recent storm snow. On Wednesday we received a report of a skier triggered size 1 wind slab on a north aspect at 1800m. It's thought that this avalanche failed on the December 9th melt freeze crust which was down 40cm at the location of the avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 1 loose natural point releases ran yesterday in steep terrain at tree line elevations. These new snow sluffs have little in the way of destructive potential. Cornices noses are very touchy. A skier accidental size 1 avalanche was observed yesterday on a convex lee feature in the alpine.&nbsp; </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Loose dry slides out of steeper unskiable terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some small natural wind slabs were reported on northern aspects in the alpine on Wednesday. On Thursday, explosives were used in the north of the region but only triggered loose sluffing from steep slopes on a variety of aspects. On Friday, ski cutting of steep convex features in the alpine produced two size 1 loose dry avalanches. New wind slabs are expected to form during the weekend storm and may be sensitive to human-triggering on Sunday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent slab avalanches have been reported. Minor sluffing from steep terrain was reported on Wednesday. On Thursday, explosives produced only loose sluffing from steep terrain features. New wind slabs are expected to form during the weekend storm and may be sensitive to human-triggering on Sunday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported since Monday.  New wind slabs are expected to form during the weekend storm and will probably be sensitive to human-triggering on Sunday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, two skier accidental avalanches were reported in the Golden backcountry. The first occurred in the morning and was a size 2 wind slab avalanche which occurred on a northwest aspect at about 2400m. It was up to 50cm in depth and ran approximately 600m. The second occurred in the afternoon and was a size 2.5 wind slab at ridgetop. This also occurred on a NW aspect at 2400m elevation. This avalanche stepped down to a deeper layer lower down in the start zone, likely the early December interface. On Thursday, a large settlement was felt in a flat meadow in the Invermere backcountry. This occurred at 2200m in a below treeline terrain feature and the failure layer is unknown. No new avalanches were reported on Friday.  New wind slabs are expected to form during the weekend storm and may be sensitive to human-triggering on Sunday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">A round of wind slab avalanche activity is expected in response to new snow and wind on Saturday night. Cornices may also continue to grow, increasing their likelihood of failure.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new activity to report from Friday. On Thursday a skier triggered an avalanche that partially buried two people in the party near 1st Pump Peak on Seymour. Details here: http://bit.ly/1MzDfHM Widespread touchy storm slabs released naturally Wednesday night with an average crown depth of 30cm. This comes on the heels of all the activity reported during the day Wednesday when the new new/old snow interface was quite touchy. On Wednesday we received multiple reports of remote triggering of small shallow storm slabs from as far away as 100m on all aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Recent explosives avalanche control in the Shames area produced several size 1.5 slab avalanches on a variety of aspects between 1250m and 1330m. A surface hoar layer buried in mid-December was the suspected culprit in these events. Moving forward, new snow and wind is expected to spark a round of destructive natural storm slab activity on all aspects and elevations. Due to underlying persistent weak layers, human triggering will remain a very real concern for several days after the storm has ended.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Boxing Day storm slab avalanches were triggered by natural cornice fall and skiers, running to size 2 on north, northeast and east facing features between 1700 and 2000m. Loose avalanches also continue to be reported. On Christmas Day natural storm slab avalanches to size 2 were reported from NE facing features between 1700 and 2050m. This comes on the heels of Thursday's activity when control work produced storm slabs up to size 1.5, with the bulk of the activity occurring on north and northeast facing slopes between 1500 and 2100m. Intentional ski cutting Thursday produced avalanches to size 1 that ran in the new storm snow. Control work Thursday also triggered one large (size 2.5) avalanche that ran on the mid-December surface hoar on an unknown aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday numerous loose dry avalanches ran naturally to size 1 on east through southeast facing features around 2250m. On Thursday control work produced numerous small loose snow avalanches within the recent storm snow. On Wednesday we received a report of a skier triggered size 1 wind slab on a north aspect at 1800m. It's thought that this avalanche failed on the December 9th melt freeze crust which was down 40cm at the location of the avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">No recent avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent avalanche activity has been limited to fast running loose snow avalanches on steep features and small wind slabs in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported.  With new snow and wind forecast for the weekend, I expect a round of wind slab activity in high elevation lee terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The storm snow has settled and gained strength, but new soft slabs have formed overnight. Expect to see loose sluffing in steep terrain, but it will have little in the way of destructive potential. Cornice tabs will be fragile</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A small avalanche cycle, up to size 1.5 was observed today along the Smith Dorrian/Spray HWY as a result of the winds yesterday and through the evening. These were predominantly thin, 10-20 cm wind slabs and most of them were on north, northeast and east aspects directly below large alpine head walls. These small slab avalanches were observed between 2400-2600 meters. Some cross-loading did occur as well but no natural avalanches were produced from the influence of the winds on these features. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, two skier accidental avalanches were reported in the Golden backcountry. The first occurred in the morning and was a size 2 wind slab avalanche which occurred on a northwest aspect at about 2400 m. It was up to 50 cm in depth and ran approximately 600 m. The second occurred in the afternoon and was a size 2.5 wind slab at ridgetop. This also occurred on a NW aspect at 2400 m elevation. This avalanche stepped down to a deeper layer lower down in the start zone, likely the early December interface. On Thursday, a large settlement was felt in a flat meadow in the Invermere backcountry. This occurred at 2200 m in a below treeline terrain feature and the failure layer is unknown. Since then, only small loose dry avalanches have been observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few size 1-1.5 loose dry avalanches have been reported over the last few days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">In the north of the region, a size 3.5 deep persistent slab failed on facets above ice, 2 m deep. This was on a steep alpine north aspect and occurred some time in the last few days. Otherwise, only loose dry avalanches, mainly size 1-1.5, have been reported over the last couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No avalanches have been reported recently in the Cariboos. In the neighbouring North Columbia region, a large natural slab failed on a deeply buried weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3428770D">On Sunday, size 1 soft wind slabs were ski cut in steep, unsupported terrain. The new avalanches formed in response to new snow and wind over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Due to inclement weather, observations were generally limited on Saturday, but a widespread storm slab cycle to size 2 was observed in the north of the region. Natural avalanche activity will likely taper-off with forecast clearing. However, human-triggered avalanches will remain a concern for the forecast period, especially at elevations or in parts of the region where recent storm accumulations have settled into a cohesive slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday ski cutting produced size 1 to 1.5 storm slabs with an average depth of 15 to 20cm. No failures below the recent snow were observed. No new activity to report from Friday or Saturday. On Thursday a skier triggered an avalanche that partially buried two people in the party near 1st Pump Peak on Seymour. Details here: http://bit.ly/1MzDfHM Widespread touchy storm slabs released naturally Wednesday night with an average crown depth of 30cm. This comes on the heels of all the activity reported during the day Wednesday when the new new/old snow interface was quite touchy and numerous small avalanches were remote triggered from as far as 100m away.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new activity to report from Saturday. Previous to this, recent avalanche activity has been limited to fast running loose snow avalanches on steep features and small wind slabs in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Boxing Day storm slab avalanches were triggered by both natural cornice fall and skiers, running to size 2 on north, northeast and east facing features between 1700 and 2000m. Loose dry avalanches also continue to be reported. On Christmas Day natural storm slab avalanches to size 2 were reported from NE facing features between 1700 and 2050m. This comes on the heels of Thursday's activity when control work produced storm slabs up to size 1.5, with the bulk of the activity occurring on north and northeast facing slopes between 1500 and 2100m. Intentional ski cutting Thursday produced avalanches to size 1 that ran in the new storm snow. Control work Thursday also triggered one large (size 2.5) avalanche that ran on the mid-December surface hoar on an unknown aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday control work and natural failure resulted in wind slabs up to size 2 on NE facing terrain at 2100m. These fresh wind slabs were failing on the Boxing Day facets. On Friday numerous loose dry avalanches ran naturally to size 1 on east through southeast facing features around 2250m. On Thursday control work produced numerous small loose snow avalanches within the recent storm snow. On Wednesday we received a report of a skier triggered size 1 wind slab on a north aspect at 1800m. It's thought that this avalanche failed on the December 9th melt freeze crust which was down 40cm at the location of the avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Isolated soft slabs have been triggered by the weight of a skier/snowboarder in lee ridge top features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new observed today, but visibility was limited. Yesterday several slab avalanches up to size 1.5 were observed on N and E aspects in steep Alpine terrain between 2400 and 2600m. These slabs were 10 to 20cm thick and generally did not run far.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new reports of avalanches. On Boxing Day storm slab avalanches were triggered by both natural cornice fall and skiers, running to size 2 on north, northeast and east facing features between 1700 and 2000m. Loose dry avalanches also continue to be reported. On Christmas Day natural storm slab avalanches to size 2 were reported from NE facing features between 1700 and 2050m. This comes on the heels of Thursday's activity when control work produced storm slabs up to size 1.5, with the bulk of the activity occurring on north and northeast facing slopes between 1500 and 2100m. Intentional ski cutting Thursday produced avalanches to size 1 that ran in the new storm snow. Control work Thursday also triggered one large (size 2.5) avalanche that ran on the mid-December surface hoar on an unknown aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several small loose dry and very soft slab avalanches have been reported over the last couple of days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">A few size 1.5 wind slabs were triggered by ski-cutting in the Duffey Lake area on Sunday. They occurred on a northwest aspect in alpine terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">In the north of the region, a size 3.5 deep persistent slab failed on facets above ice, 2 m deep. This was on a steep alpine north aspect and occurred some time in the last few days. Otherwise, only loose dry avalanches, mainly size 1-1.5, have been reported over the last couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday a group of sledders triggered or remotely triggered an avalanche &quot;near&quot; Castle Mountain that resulted in one rider deploying his airbag and being partially buried; the size of the slab avalanche was not reported. See the MIN report for more information. On Saturday, in the east of the region, control work and natural avalanches resulted in wind slab releases up to size 2 on NE facing terrain at 2100m. These fresh wind slabs were failing on the Boxing Day facets. On Friday numerous loose dry avalanches ran naturally to size 1 on east through southeast facing features around 2250m. On Thursday control work produced numerous small loose snow avalanches within the recent storm snow. On Wednesday we received a report of a skier triggered size 1 wind slab on a north aspect at 1800m. It's thought that this avalanche failed on the December 9th melt freeze crust which was down 40cm at the location of the avalanche.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Sunday and Monday, size 1 soft wind slabs were ski cut in steep, unsupported terrain. The new avalanches formed in response to new snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Apart from loose sluff and whumpfing, no avalanches have been reported recently. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported&nbsp; On Sunday ski cutting produced size 1 to 1.5 storm slabs with an average depth of 15 to 20cm. No failures below the recent storm snow were observed. No new activity to report from Friday or Saturday. On Thursday a skier triggered an avalanche that partially buried two people in the party near 1st Pump Peak on Seymour. Details here: http://bit.ly/1MzDfHM Widespread touchy storm slabs released naturally Wednesday night with an average crown depth of 30cm. This comes on the heels of all the activity reported during the day Wednesday when the new new/old snow interface was quite touchy and numerous small avalanches were remote triggered from as far as 100m away.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, two avalanches were triggered by skiers in the Golden backcountry. The first was a size 2 wind slab which occurred on a northwest aspect at about 2400 m. It was up to 50 cm in depth and ran approximately 600 m. The second was a size 2.5 wind slab at ridgetop. This also occurred on a NW aspect at 2400 m elevation. This avalanche stepped down to a deeper layer lower down in the start zone, likely the early December interface. On Thursday, a large settlement was felt in a flat meadow in the Invermere backcountry. This occurred at 2200 m in a below treeline terrain feature and the failure layer is unknown. Since then, several small loose dry avalanches and one size 1.5 wind slab have been observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Evidence of natural storm slab avalanches to size 2 was observed in the wake of Saturday's storm. In sheltered terrain, loose dry avalanche activity has also been noted. Natural avalanche activity will likely taper-off with the current clearing trend. However, human-triggered avalanches will remain a concern for the forecast period, especially at elevations or in parts of the region where recent storm accumulations have settled into a cohesive slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There is a great deal of variability across the region. The southern Monashees have reported 40 cm deep soft slabs that are easy to trigger and likely to entrain loose dry snow in avalanche tracks and runouts. As you move east across the region the storm slab depths become less, with about 20 cm in the Rossland range, and closer to 10 cm of recent snow 40-50 cm of overall storm snow in the Kootenay pass.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Isolated soft slabs have been triggered by the weight of a skier/snowboarder in lee ridge top features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several small wind slab avalanches up to size 1.5 have occurred on steep N, NE and E aspects in the Alpine over the past 72 hours. These slides are between 10 and 20cm thick and have generally not run very far down slope.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported since Saturday. I suspect pockets of storm snow may continue to be triggered at higher elevations in the lee of terrain features. Forecast solar radiation may consolidate the recent storm snow into a cohesive slab and allow for longer fracture propagations on isolated wind loaded pockets. Loose moist or wet slides may occur in steep terrain if solar radiation is strong enough.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. There is a great deal of variability across the region. The southern Monashees have reported 40 cm deep soft slabs on Monday that are easy to trigger and likely to entrain loose dry snow in avalanche tracks and runouts. One ski cut stepped down to a weak layer buried about 100 cm according to a MIN report. As you move east across the region the storm slab depths become less, with about 20 cm in the Rossland range, and closer to 10 cm of recent snow 40-50 cm of overall storm snow in the Kootenay pass.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Over the last few days, several small loose dry avalanches and one size 1.5 wind slab have been observed. Persistent slabs were last triggered about a week ago. Unfortunately these types of problems don't heal quickly, so they remain on our radar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several small loose dry and very soft slab avalanches have been reported over the last couple of days. </span><span class="s_3D0464D1">A touch of sun and warming may spark some loose natural avalanches or create slab properties in the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new reports of natural avalanches. A commercial operation reported explosive control work released a cornice to size 1.5 on a N-NE aspect at 2050 metres elevation on Tuesday, and another operation reported skier controlled slab avalanches up to size 1.5 on Monday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">A few wind slabs up to size 1.5 were triggered by ski-cutting in the north of the region on Sunday. They occurred on a northwest aspect in alpine terrain. With solar radiation and warmer alpine temperatures forecast for the next few days, loose wet avalanches may occur on steep, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Several loose dry and soft slab avalanches, mainly size 1-1.5, have been reported over the last couple of days. Many have been on recently wind-loaded terrain features. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Evidence of natural storm slab avalanches to size 2 was observed in the wake of Saturday's storm. Natural avalanche storm slab activity has tapered-off with the current clearing trend. However, human-triggered avalanches will remain a concern for the forecast period, especially at elevations or in parts of the region where recent storm accumulations have settled into a cohesive slab. Small solar-induced loose wet avalanches have also been reported. The likelihood and size of loose wet avalanches will increase with warmer alpine temperatures expected during the forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A skier triggered a size 1 soft slab on a NW aspect and a size 2 glide slab release was observed at 1200 m. Otherwise, there has been little avalanche activity reported recently. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported. With solar radiation and slight warming forecast for the next few days, loose wet avalanches will become more likely on steep, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Monday, size 1 soft wind slabs were ski cut in steep, unsupported alpine terrain. The new avalanches formed in response to new snow and wind. Small solar-induced loose wet avalanches have also been reported. The size and likelihood of loose wet avalanches will increase with warmer alpine temperatures expected during the forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday a group of sledders triggered or remotely triggered a slab avalanche size 2.0 about 2km south of Castle Mountain that resulted in one rider deploying his airbag and being partially buried. See the MIN report for more information. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Isolated soft slabs have been triggered by the weight of a skier/snowboarder in lee/cross loaded alpine  features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported since Saturday. I suspect pockets of storm snow may continue to be triggered at higher elevations in the lee of terrain features. Forecast solar radiation may consolidate the recent storm snow into a cohesive slab and allow for longer fracture propagations on isolated wind loaded pockets. Loose moist or wet slides may occur in steep terrain if solar radiation is strong enough.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday quite of a bit of slufing/loose dry activity was reported to size 1. These small natural avalanches were running in the upper 10cm of the snowpack. There is a great deal of variability across the region. The southern Monashees reported 40 cm deep soft slabs on Monday that were easy to trigger and entrained loose dry snow in avalanche tracks and runouts. One ski cut stepped down to a weak layer buried about 100cm deep according to a MIN report. (http://bit.ly/1Sn9Do7) As you move east across the region the storm slab depths become less, with about 20 cm in the Rossland range, and closer to 10 cm of recent snow, 40-50 cm of overall storm snow in the Kootenay pass.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Several small loose dry avalanches, small soft slab avalanches, and cornice releases have been reported over the last couple of days. Progressive warming in the alpine with ongoing sunny conditions should result in ongoing loose natural avalanches from south-facing slopes and by the weekend may create slab properties within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several small loose dry avalanches, small soft slab avalanches, and cornice releases have been reported over the last couple of days. Progressive warming in the alpine with ongoing sunny conditions should result in ongoing loose natural avalanches from south-facing slopes and by the weekend may create slab properties within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural and explosive triggered cornice failures to size 1.5 were reported on N/NE facing alpine features Tuesday. On Monday skier controlled slab avalanches up to size 1.5 were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity to report from the last 3 days.. On Sunday a group of sledders triggered or remotely triggered a slab avalanche size 2.0 about 2km south of Castle Mountain that resulted in one rider deploying his airbag and being partially buried. More details here: http://bit.ly/1TqhuQf</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a skier triggered a size 1 soft slab on a NW aspect and a size 2 glide slab release was observed at 1200 m. On Tuesday, several size 1 wind slabs were ski cut on SE through SW aspects in the alpine.  This were typically soft slabs 5-30cm thick.  Progressive warming in the alpine with ongoing sunny conditions should result in ongoing loose natural avalanches from south-facing slopes and by the weekend may create slab properties within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the last few days, several small loose dry avalanches and one size 1.5 wind slab have been observed. Persistent slabs were last triggered about a week ago. Unfortunately these types of problems don't heal quickly, so they remain on our radar. This problem may wake up with the upcoming warm temperatures in the alpine.&nbsp; Progressive warming in the alpine with ongoing sunny conditions should result in ongoing loose natural avalanches from south-facing slopes and by the weekend may create slab properties within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported. With solar radiation and warmer alpine temperatures forecast for the next few days, loose wet avalanches may occur on steep, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Tuesday a size 1-1.5 skier-triggered wind slab avalanche was observed in Body Bag Bowl in the Spearhead Range. The rider went for a 30m ride and lost a pole, but did not sustain any injuries. On the same day, a size 1.5 slab avalanche was triggered on Rainbow Mountain. The avalanche, which occurred on a lower-elevation northeast facing slope, is thought to have failed on the mid-December surface hoar. For great photos of these slides, check-out Wayne Flann's Avalanche Blog at: http://www.wayneflannavalancheblog.com/2015/12/december-30-2015.html </span></p><p class="p_CC664AAA"><span class="s_A8FEC758">On Wednesday, there was a report of a rider-triggered size 1 wind slab avalanche near Adit Lakes in the Fitzsimmons Range. The avalanche occurred on a northwest facing slope at 1950m. Small solar-induced loose wet avalanches have also been reported. The size and likelihood of loose wet avalanches will increase with warmer alpine temperatures expected during the forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Natural avalanche storm slab activity has tapered-off with the current clearing trend. However, human-triggered avalanches will remain a concern for the forecast period, especially at elevations or in parts of the region where recent storm accumulations have settled into a cohesive slab. Solar-induced loose wet avalanches up to size 1.5 have also been reported. The likelihood and size of loose wet avalanches will increase with warmer alpine temperatures expected during the forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No recent avalanches have been reported. With solar radiation and warming forecast for the next few days, loose wet avalanches will become more likely on steep, sun-exposed slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Small loose wet natural avalanches are likely from steep SE through SW facing alpine start zones as the sun adds its warmth to the snow. Isolated soft slabs have been triggered by skier/snowboarder's in lee and cross loaded alpine features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasters witnessed a skier accidental today in alpine terrain. The feature was just below a pinch in a large alpine gully. The small slab avalanche triggered above the person and entrained a large amount of loose snow as it made its way downhill. Sz 2, 2700m, ran 400m vertical, SE aspect. There were also continuous loose dry avalanches pouring down high alpine gullies for most of the day. These were attributed to constant windloading and in some cases solar input.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday a size 1-1.5 skier-triggered wind slab avalanche was observed in Body Bag Bowl in the Spearhead Range. The rider went for a 30m ride and lost a pole, but did not sustain any injuries. On the same day, a size 1.5 slab avalanche was triggered on Rainbow Mountain. The avalanche, which occurred on a lower-elevation northeast facing slope, is thought to have failed on the mid-December surface hoar. On Wednesday, there was a report of a rider-triggered size 1 wind slab avalanche near Adit Lakes in the Fitzsimmons Range. The avalanche occurred on a northwest facing slope at 1950m. Small solar-induced loose wet avalanches have also been reported. The size and likelihood of loose wet avalanches will increase with warmer alpine temperatures expected during the forecast period.</span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. With solar radiation and warmer alpine temperatures forecast for the next few days, loose wet avalanches may occur on steep, sun-exposed slopes.</span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No recent avalanches have been reported. With solar radiation and warming forecast for the next few days, loose wet avalanches will become more likely on steep, sun-exposed slopes.</span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural avalanche storm slab activity has tapered-off with the current clearing trend. However, human-triggered avalanches will remain a concern for the forecast period, especially at elevations or in parts of the region where recent storm accumulations have settled into a cohesive slab. Solar-induced loose wet avalanches up to size 1.5 have also been reported. The likelihood and size of loose wet avalanches will increase with warmer alpine temperatures expected during the forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Several small loose dry avalanches, small soft slab avalanches, and cornice releases have been reported over the last couple of days. Progressive warming in the alpine with ongoing sunny conditions could result in ongoing loose natural avalanches from south-facing slopes and by the weekend may create slab properties within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, a skier triggered a size 2.5 slab on a NW aspect at about 2500 m near Golden. It is thought to have failed on the early Dec persistent weak layer, down 30-60 cm. There has also been activity clustered in a region to the west of Kimberley. On Tuesday, a skier triggered a size 2 persistent slab. Last Sunday, a skier triggered a size 3 slab. Skiers also remotely triggered a size 2 slab the week before. These all failed on the early December surface hoar layer and were on all aspects between 1600 m and 2100 m. Small loose dry avalanches and cornice falls have also been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a skier triggered a size 1 soft slab on a NW aspect and a size 2 glide slab release was observed at 1200 m. On Tuesday, several size 1 wind slabs were ski cut on SE through SW aspects in the alpine. This were typically soft slabs 5-30 cm thick. Progressive warming in the alpine with ongoing sunny conditions should result in ongoing loose natural avalanches from south-facing slopes and by the weekend may create slab properties within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several small loose dry avalanches, small soft slab avalanches, and cornice releases have been reported over the last few days. Progressive warming in the alpine with ongoing sunny conditions should result in ongoing loose natural avalanches from south-facing slopes and by the weekend may create slab properties within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported since Saturday. I suspect pockets of storm snow may continue to be triggered at higher elevations in the lee of terrain features. Forecast solar radiation and warm temperatures may consolidate the recent storm snow into a cohesive slab and allow for longer fracture propagations on isolated wind loaded pockets. Loose moist or wet slides may occur in steep terrain if solar radiation is strong enough.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday and Wednesday quite of a bit of slufing/loose dry activity was reported to size 1. These small natural avalanches were running in the upper 10cm of the snowpack. There is a great deal of variability across the region. The southern Monashees reported 40 cm deep soft slabs on Monday that were easy to trigger and entrained loose dry snow in avalanche tracks and runouts. One ski cut stepped down to a weak layer buried about 100cm deep according to a MIN report. (http://bit.ly/1Sn9Do7) As you move east across the region the storm slab depths become less, with about 20 cm in the Rossland range, and closer to 10 cm of recent snow, 40-50 cm of overall storm snow in the Kootenay pass.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday control work produced a size 2 storm slab on a high elevation east facing feature. Previous to this, the last reported avalanche activity was on Sunday when a group of sledders triggered or remotely triggered a slab avalanche size 2.0 about 2 km south of Castle Mountain that resulted in one rider deploying his airbag and being partially buried. More details here: http://bit.ly/1TqhuQf</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday one small loose dry avalanche was reported on a NE facing feature at treeline. Natural and explosive triggered cornice failures to size 1.5 were reported on N/NE facing alpine features Tuesday. On Monday skier controlled slab avalanches up to size 1.5 were reported.</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">No new avalanche activity was noted on Friday but observations were limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Several small loose dry avalanches, small soft slab avalanches, and 1 large glide-crack release have been reported over the last couple of days. Continued warming in the alpine combined with sunny conditions could result in loose natural avalanches from steep south-facing slopes. Recent storm snow will begin to show slab properties as it settles with the warm temperatures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Earlier in the week there were reports of skier triggered soft slabs up to size 1.5 These were mostly soft slabs 5-30 cm thick. Progressive warming in the alpine with sunny conditions may result in loose natural avalanches on steep south-facing slopes. Continued warming through the weekend may create a denser slab within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Several loose dry avalanches, small soft slab avalanches, and 1 large glide release were reported yesterday. Progressive warming in the alpine with sunny conditions will result in loose natural avalanches from steep south-facing slopes. Recent new snow will become more slab-like with the mild temperatures.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Thursday, a skier triggered a size 2.5 slab on a NW aspect at about 2500 m near Golden. It is thought to have failed on the early Dec. persistent weak layer, down 30-60 cm. There has also been activity clustered in a region to the west of Kimberley. On Tuesday, a skier triggered a size 2 persistent slab. Last Sunday, a skier triggered a size 3 slab. Skiers also remotely triggered a size 2 slab the week before. These all failed on the early December surface hoar layer and were on all aspects between 1600 m and 2100 m. Small loose dry avalanches and cornice falls have also been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715"> Solar induced loose snow avalanches have released naturally up to size 1.5 in may areas, and one south aspect size 2.0 avalanche was reported from the Wedge on Thursday. Explosives control late in the day on Thursday, released some &quot;sizeable chunks&quot; of cornice that propagated the storm snow on the slope below; size not reported. Some skier controlled pockets of wind slab 20-40 cm deep and up to size 1.0 were also reported on Thursday in the Whistler area.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some isolated skier controlled soft wind slabs released from immediate lee features in the north of the region. No new avalanches reported from the south of the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">One skier accidental size 1.5 avalanche was reported from the north of the region on Thursday. The avalanche was a wind slab on an east aspect at 1200 metres that was 20-60 cm deep and released on a buried surface hoar layer from mid-December.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported. Commercial operations cautioning new wind slabs at ridge lines developing with outflow winds. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported since Saturday, but we suspect loose moist and/or wet slides may be occurring in steep terrain when solar radiation is at it's peak.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, Wednesday and Thursday activity has been limited to small loose snow avalanches running in the upper snowpack. There is probably more of this activity on solar aspects than the more shady north and east aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday a size 2 wind slab was triggered by explosive control work on a steep north facing feature around 2000m. Numerous loose dry avalanches failed naturally as solar aspects were kissed by the sun. On Thursday loose dry avalanches to size 1 were reported on solar aspects at and above treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday control work produced loose dry avalanches to size 1 on E and NE aspects. On Wednesday control work produced a size 2 storm slab on a high elevation east facing feature. Previous to this, the last reported avalanche activity was on Sunday when a group of sledders triggered or remotely triggered a slab avalanche size 2.0 about 2 km south of Castle Mountain that resulted in one rider deploying his airbag and being partially buried. More details here: http://bit.ly/1TqhuQf</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Isolated soft slabs have been triggered by skier's/snowboarder's in lee and cross loaded alpine features. Small loose wet natural avalanches have been triggered from steep SE through SW facing alpine start zones by the warm temperatures and direct solar exposure. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new today, but a skier accidentally triggered a size 2.0 wind slab avalanche a couple of days ago in steep Alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Solar-induced loose wet avalanches to size 1.5 released naturally over the last few days in response to solar radiation and warming at higher elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some isolated skier controlled soft wind slabs released from immediate lee features in the north of the region. I'm sure there was also some loose wet avalanche activity on steep, sun-exposed terrain with warm alpine temperatures and solar radiation over the past few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Aside from a few size 1 wind slab avalanches in the far north of the region, no new avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous reports of loose dry avalanches up size 2.5 originating from steep solar aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">A few reports from yesterday speak of loose, dry sluffing from steep solar affected alpine slopes. Otherwise, no avalanche activity to report.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports of loose natural avalanches on steep south-facing slopes. Continued warming through the weekend may create a denser slab within the recent storm snow.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Reports from yesterday indicate that loose-dry natural avalanches ( up to size 2.5 ) out of steep solar affected slopes remain a prime concern. There has also been reported a large, loose-dry avalanche from a North East facing slope in the alpine. Earlier in the week several large avalanches were triggered in the southern Purcells, west of Kimberly, on buried surface hoar. Something to keep in mind when looking for new terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">One skier accidental size 1.5 avalanche was reported from the north of the region on Thursday. The avalanche was a wind slab on an east aspect at 1200 metres. It was 20-60 cm deep, and released on a buried surface hoar layer from mid-December.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches reported since Saturday, but we suspect that loose moist and/or wet slides may have occurred during the peak of the warming and solar radiation over the last 72 hours.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday control work produced loose dry avalanches to size 1 on E and NE aspects. On Wednesday control work produced a size 2 storm slab on a high elevation east facing feature. Previous to this, the last reported avalanche activity was on Sunday when a group of sledders triggered or remotely triggered a large slab avalanche about 2 km south of Castle Mountain that resulted in one rider deploying his airbag and being partially buried. More details here: http://bit.ly/1TqhuQf</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday a size 2 wind slab was triggered by explosive control work on a steep north facing feature around 2000m. Numerous loose dry avalanches failed naturally as solar aspects were kissed by the sun. On Thursday loose dry avalanches to size 1 were reported on solar aspects at and above treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">For the last four days reported avalanche activity has been limited to small loose snow avalanches running in the upper snowpack. There has probably been more of this activity on solar aspects than the more shady north and east aspects. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B"> Cornices have been touchy over the past few days. There were a few reports of small slab avalanches last week, but those events seem to have slowed down for the moment.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Over the weekend there were avalanches observed up to size 2.0 loose wet and loose dry in the Rockies.  The cooler temperatures have returned and avalanche activity has slowed since.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently but we suspect that loose moist and/or wet slides may have occurred during the sun and warming over the last few days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been observed. Looking forward, new wind slab activity is expected in higher elevation lee terrain over the next few days. The expected size and distribution of new wind slab avalanches is really tough to pin down at this point due to uncertainty in the weather forecast.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Reports of loose natural avalanches on steep south-facing slopes up to size 1.5 .</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous reports of loose dry avalanches up size 2.5 originating from steep solar aspects, and a report of a skier controlled size 1, wind slab on a northern aspect</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Reports of loose dry avalanches up size 2.5 originating from steep solar aspects, and a report of a size 1, natural wind slab on an eastern aspect.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend, avalanche activity has been limited to small loose snow avalanches running in the upper snowpack. Sun exposed slopes likely saw the most avalanche activity but reports suggest that sluffing occurred on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Loose-dry natural avalanches ( up to size 1.5 ) out of steep solar affected slopes are still being reported.  Earlier in the week several large avalanches were skier triggered in the southern Purcells, west of Kimberly, on buried surface hoar. Something to keep in mind when looking for new lines!</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, a skier triggered a size 1 wind slab avalanche on a NE aspect at 1850m elevation.  The wind slab was 10cm thick.  Explosives triggered several cornice releases on north through east aspects between 1950m and 2100m.  Four of these cornice releases triggered small storm slabs on the slopes below which were limited to around 20cm thickness. On Friday, a size 2 wind slab was triggered by explosive control work on a steep north facing feature around 2000m. Numerous loose dry avalanches failed naturally as solar aspects were kissed by the sun. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been observed. Looking forward, new wind slab activity is expected in higher elevation lee terrain over the next few days. The expected size and distribution of new wind slab avalanches is really tough to pin down at this point due to uncertainty in the weather forecast.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported over the weekend but sluffing is expected to have occurred on steep south facing slopes. On Friday control work produced loose dry avalanches to size 1 on E and NE aspects. On Wednesday control work produced a size 2 storm slab on a high elevation east facing feature. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has been some very isolated windslab activity over the past few days. The surface instabilities have stabilized with the cooling temperatures. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Little avalanche activity has been observed in K-Country or from our nearest neighbors in Banff National Park, Sunshine Ski Area or Lake Louise.  Isolated loose dry avalanches up to 1.5.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some loose snow avalanches continue to be reported from steep alpine terrain. Last week several large avalanches were skier triggered in the southern Purcells, west of Kimberly, on buried surface hoar. Something to keep in mind when looking for new lines!</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been observed. Looking forward, new wind slab activity is expected in higher elevation lee terrain over the next few days. The expected size and distribution of new wind slab avalanches is really tough to pin down at this point due to uncertainty in the weather forecast.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Some isolated wind slab avalanches reported up to size 1.5</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">In the last few days, a natural cornice fall on Decker Mountain in the Spearhead Range triggered a size 1.5 wind slab on a northwest facing alpine feature. Looking forward, new wind slab activity is expected in higher elevation lee terrain over the next few days. The expected size and distribution of new wind slab avalanches is really tough to pin down at this point due to uncertainty in the weather forecast.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some thin wind slabs avalanches size 1.0 were reported that were about 10 cm deep.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently but we suspect that loose moist and/or wet slides may have occurred during the sun and warming over the last few days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported over the weekend but sluffing is expected to have occurred on steep south facing slopes. On Friday control work produced loose dry avalanches to size 1 on E and NE aspects. On Wednesday control work produced a size 2 storm slab on a high elevation east facing feature. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, a skier triggered a size 1 wind slab avalanche on a NE aspect at 1850m elevation. The wind slab was 10cm thick. Explosives triggered several cornice releases on north through east aspects between 1950m and 2100m. Four of these cornice releases triggered small storm slabs on the slopes below which were limited to around 20cm thickness. On Friday, a size 2 wind slab was triggered by explosive control work on a steep north facing feature around 2000m. Numerous loose dry avalanches failed naturally as solar aspects were kissed by the sun. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, a few avalanches were reported from the north of the region: A skier accidentally triggered a size 1.5 wind slab avalanche which failed on the December 26 surface hoar layer at about 1450m on an east aspect. A few other size 1.5 explosive-triggered wind slabs were also observed in north-facing alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity has been limited to small loose snow avalanches running in the upper snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There has been some isolated wind slab activity during the past week that has diminished over the past several days. Expect to see some wind loaded areas today with size 1.0 soft slabs that are reactive to the weight of a person.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new in the past 48hrs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Loose snow sluffing in steep terrain continues to be reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some wind slab avalanches have been reported up to size 1.0 in the alpine. Skiers sluff running fast on recently buried surface hoar and facets.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, three avalanches were reported north of Stewart but details were limited.  A natural size 2 wind slab had a thickness of 100cm.  A snowcat triggered a size 1.5 wind slab 35cm thick and a ski cut produced a size 1 wind slab 25cm thick.  These were likely formed by outflow winds mean they were probably on west or southwest aspects.  On Sunday, a few avalanches were reported from the north of the region: A skier accidentally triggered a size 1.5 wind slab avalanche which failed on the December 26 surface hoar layer at about 1450m on an east aspect. A few other size 1.5 explosive-triggered wind slabs were also observed in north-facing alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some thin wind slabs avalanches size 1.0 were reported that were about 10 cm deep.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new natural avalanches reported. Some loose snow avalanches up to size 1.0 continue to be reported from steep shaded aspects in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new slab avalanches have been reported. Skier triggered sluffing was reported from steep terrain in the far north of the region on Monday.</span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported since the weekend. On Saturday, a natural cornice fall on Decker Mountain in the Spearhead Range triggered a size 1.5 wind slab on a northwest facing alpine feature. Looking forward, new wind slab activity is expected in higher elevation lee terrain over the next couple days but these wind slabs are generally expected to be small and thin.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, a skier triggered a size 1 wind slab avalanche on a NE aspect at 1850m elevation. The wind slab was 10cm thick. Explosives triggered several cornice releases on north through east aspects between 1950m and 2100m. Four of these cornice releases triggered small storm slabs on the slopes below which were limited to around 20cm thickness. On Friday, a size 2 wind slab was triggered by explosive control work on a steep north facing feature around 2000m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported over the weekend but sluffing is expected to have occurred on steep south facing slopes. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported recently but I suspect that wind loaded features are touchy</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Avalanche activity has been limited to small loose snow avalanches running in the upper snowpack.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">You can expect to see areas of soft slabs up to size 1.5 that will be reactive to the weight of a person in some wind loaded terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were noted today/  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Thin new windslabs were reported releasing up to size 1.0 in the north of the region. One third hand report of a remotely triggered size 2.0 wind slab on a North aspect at 2440 metres near Panorama.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural cornice avalanches and natural and skier controlled wind slab avalanches up to size 1.5 have been reported. Most of these have been on northerly aspects in the lee of local winds. Winds have been generally easterly, but some areas have had locally more southerly winds due to terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Minimal sluffing in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some thin wind slabs avalanches size 1.0 were reported that were about 10 cm deep. Loose dry snow sluffing in steep terrain on northerly aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new slab avalanches have been reported. Loose snow sluffing up to size 1.5 from steep terrain in the northwest of the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some natural wind slab activity size 2.0 was reported from the north of the region near the coast where the outflow winds were reported to be strong. There have been no reports of avalanches from the ski operations in the south or from MIN reports.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported recently but I suspect that wind loaded features are still touchy</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Saturday, a skier triggered a size 1 wind slab avalanche on a NE aspect at 1850m elevation. The wind slab was 10cm thick. Explosive avalanche control also triggered several cornice releases on north through east aspects between 1950m and 2100m. Four of these cornice releases triggered small slabs on the slopes below which were limited to around 20cm thickness.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Reports suggest that the layer of buried surface hoar is starting to wake up especially in the south west of the region where overlying snow load above is greatest. Small natural avalanche were reported in steep open features at treeline on Tuesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Small soft wind slabs were reported on lee slopes at alpine elevations near Whistler on Tuesday afternoon. I expect warm temperatures should help these slabs settle in place rather quickly.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">You can expect to see size 1.0 soft slabs that will be reactive to the weight of a person in some wind loaded terrain. Solar induced surface instabilities can also be expected to develop by midday on easterly aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">The only recent reports of avalanche activity have been small loose dry avalanches out of steep rocky north facing terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Natural cornice avalanches and natural and skier controlled wind slab avalanches up to size 1.0 have been reported. Most of these have been on northerly aspects in the lee of local winds. Winds have been generally easterly, but some areas have had locally more southerly winds due to terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new natural avalanches reported. Explosive cornice control did not release a slab on slopes below.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Minimal sluffing in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some thin wind slabs avalanches size 1.0 were reported that were about 10-30 cm deep. Loose dry snow sluffing in steep terrain on northerly aspects. One natural ice fall size 2.5 was reported from the Selkirks that entrained some loose snow but did not trigger a slab avalanche. One natural size 2.0 was reported from the Monashees, that was seen from a distance and the observer was not sure of the details.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose dry sluffs out of steep south terrain. Up to sz1. Likely because of a suncrust on those aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Small natural, skier controlled, avalanches have been reported from steep open features at treeline.&nbsp; There was also a report of a size 2 skier remotely triggered wind slab on a steep north aspect in the alpine near Nelson on Thursday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some recent natural wind slab activity to size 2.0 was reported from the north of the region near the coast where the outflow winds were reported to be strong. There have been no reports of avalanches from the ski operations in the south or from MIN reports.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new slab avalanches have been reported. Loose snow sluffing up to size 1.5 has been reported from steep terrain in the northwest of the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Small soft wind slabs were reported on lee slopes at alpine elevations near Whistler on Tuesday and Wednesday. I expect warmer temperatures should help these slabs settle in place rather quickly.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches were reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">You can expect to see size 1.0 soft slabs that may remain reactive to the weight of a person in some isolated wind loaded terrain. Small solar induced surface instabilities can also be expected to develop by midday on easterly aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Several loose dry avalanches (up to sz 1.5) were noted on N to S aspects today. A natural sz2 slab was noted on Mt Engadine. It was on a SW aspect, started in an alpine feature and entrained the facetted layers underneath. The suspected failure plain is a thin suncrust from the warm spell last week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Minimal sluffing in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There was a natural size 2.0 avalanche in the alpine on a south aspect in the Selkirks that was seen from a distance and may have been wind slab. Some sluffing in steep terrain continues to be reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Explosive avalanche control produced numerous storm slab avalanches up to size 2 around Nelson on Thursday. There was also a report of a size 2 skier remotely triggered wind slab on a steep north aspect in the alpine. Earlier in the week numerous small natural and skier controlled avalanches were reported from steep open features at treeline. All of these avalanches have been failing on the recently buried layer of surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some loose snow sluffing in steep terrain had been reported up to size 1.5. Loose snow in a gully feature caused one skier to be caught in a size 1.5 avalanche. Sluff management is important if you are considering travelling in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported recently although several large avalanche were reported from around Fernie on thursday failing on a layer of surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new natural avalanches reported. Some sluffing reported in steep terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Thursday saw natural, accidental and explosive controlled avalanches in the Lizard Range up to size 2. The failure plan was reported as surface hoar. At this time I am uncertain as to whether these avalanches ran on the early-January or mid-December weak layer </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A couple accidentally triggered slabs up to size 1.5 were reported on Thursday. These were from exposed cross-loaded slopes in the alpine. Otherwise only small loose snow avalanches were reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported but watch for loose snow sluffing in steep terrain and sun-exposed slopes, and small wind slabs in lee and cross-loaded terrain in the alpine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanche activity has been reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">You can expect to see size 1.0 soft slabs that may remain reactive to the weight of a person in some isolated wind loaded terrain.&nbsp; A few small size 1 soft slab avalanches were observed yesterday outside the ski area boundary above 2300m.&nbsp;  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose dry and thin slab avalanche activity up to size 2.0 in the forecast region was observed on solar and polar aspects in the last 48 hours.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, several soft wind slab avalanches were ski cut in the Fernie area.&nbsp; These occurred on east aspects at 1800-2100m elevation and were in immediate leeward features around ridge crests. These slabs were 20-40cm thick and were failing on a layer of surface hoar.&nbsp; Several natural loose dry avalanches were also reported in the region and some of these loose avalanches triggered soft wind slabs up to size 2 on the slopes below.&nbsp; Thursday saw natural and explosive controlled storm slab avalanches up to size 2. These were mainly failing on the early January surface hoar layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported but watch for loose snow sluffing in steep terrain and sun-exposed slopes, and small wind slabs in lee and cross-loaded terrain in the alpine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose snow sluffing has been observed in steep terrain, but no new slab avalanches have been reported since Wednesday last week. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported but watch for loose snow sluffing in steep terrain and sun-exposed slopes, and small wind slabs in lee and cross-loaded terrain in the alpine. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of small storm slabs were triggered by skiers on Friday below treeline. These failed on buried surface hoar. Some loose dry activity has also been noted. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A cycle of naturally-triggered size 1-2 loose dry avalanches was reported on Friday. Most were on steep alpine shady aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A few small natural and rider-triggered wind slab avalanches up to size 1.5 were reported on Thursday and Friday. These were from steep East-facing slopes immediately lee of ridges. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. A size 1 cornice failed, but did not trigger a slab. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few small wind slabs were been triggered naturally on various aspects in alpine terrain on Friday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, a skier triggered a size 1 storm slab on a steep convex roll at 1700m on a north aspect.&nbsp; The slab was reported to be 28cm thick and failing on the early January surface hoar layer.&nbsp; Several loose dry avalanches up to size 1.5 were also reported on all aspects between 1900-2300m.&nbsp; On Thursday, explosive control produced numerous storm slab avalanches up to size 2 around Nelson. There was also a report of a size 2 skier remotely triggered wind slab on a steep north aspect at 2200m. This was triggered from 5m away and failed on the early January surface hoar layer down 38cm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported recently but several avalanches were reported in the Lizard region on Thursday and Friday. The primary problem in that region is wind slabs failing on the early January layer of surface hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated size 1.0 soft slabs may remain reactive to the weight of a person in some isolated wind loaded terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new observed today, but a few avalanches up to size 1.5 (both loose dry and wind slabs) have occurred in the past 72hrs in steep Alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. A size 1 cornice failed on Friday, but did not trigger a slab. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A few size 1-1.5 wind slabs and loose dry avalanches have been reported over the last two days. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A couple of small storm slabs were triggered by skiers on Friday below treeline. These failed on buried surface hoar. Some size 1 loose dry and wind slab activity has also been noted. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">A cycle of naturally-triggered size 1-2 loose dry avalanches was reported on Friday. Most were on steep alpine shady aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Saturday. A few small natural and rider-triggered wind slab avalanches up to size 1.5 were reported on Thursday and Friday from steep lee features.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday and Saturday, several soft wind slab avalanches were ski cut in the Fernie area. These slabs were 20-40cm thick and were failing on the recently buried layer of surface hoar. Several natural loose dry avalanches were also reported in the region and some of these loose avalanches triggered soft wind slabs up to size 2 on the slopes below. Thursday saw natural and explosive controlled storm slab avalanches up to size 2. These were also mainly failing on the early January surface hoar layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Saturday triggered a size 1 wind slab in the south of the region. No other recent avalanches have been reported in the South Rockies region. Several avalanches were reported in the Lizard/Flathead region on Thursday and Friday. The primary problem in that region is wind slabs failing on the early January surface hoar layer. Similar conditions may exist in some parts of the South Rockies.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some minor loose snow sluffing has been observed but there are no new reports of slab avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose snow sluffing has been observed in steep terrain, but no new slab avalanches have been reported since Wednesday last week. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported for several days; however, observations are very limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days we've received a quite few reports of skier-triggered storm slabs in the size 1-2 range from the Nelson area. In one case, a size 2 storm slab was remotely triggered from a distance of 5 metres. Recently buried surface hoar was the culprit in all of these avalanches. Storm slab avalanches are expected to increase in size and reactivity with snowfall forecast for later in the week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated size 1.0 soft slabs may remain reactive to the weight of a person in some isolated wind loaded terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No field trip today, but suspect no natural avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous loose dry avalanches up to size 1.5 occurred from steeper terrain features, especially when the sun poked out at higher elevations above the valley clouds. With forecast light, low density snow, loose dry and isolated wind slab problems will likely continue. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">The incoming storm will likely spark a widespread round of storm slab activity at elevations where precipitation falls as snow. At elevations where heavy rain falls, loose wet avalanches are possible.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. With new snow accompanied by strong winds, loose dry and isolated wind slab problems may persist through the forecast period.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Saturday triggered a size 1 wind slab in the south of the region. No other recent avalanches have been reported in the South Rockies region. Several avalanches were reported in the Lizard/Flathead region on Thursday and Friday. The primary problem in that region is wind slabs failing on the early January surface hoar layer. Similar conditions may exist in some parts of the South Rockies.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the past few days we've received a quite few reports of skier-triggered storm slabs in the size 1-2 range from the Nelson area. In one case, a size 2 storm slab was remotely triggered from a distance of 5 metres. Recently buried surface hoar was the suspected culprit in all of these avalanches. Storm slab avalanches are expected to increase in size and reactivity with snowfall forecast for later in the week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Sunday there was numerous reports of loose dry sluffing up to size 1.5, most seemed to be solar induced at higher elevations. With new snow forecast,  loose dry and storm slab avalanches could become more of a widespread problem. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Sunday, a natural icefall off a hanging glacier occurred, size 2 but did not pull a slab from the slope below. A cycle of naturally-triggered size 1 loose dry avalanches from steeper terrain features were also reported. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days, several soft wind slab avalanches in the size 1-1.5 range were ski cut in the Lizard Range. These slabs were 20-40cm thick and were failing on the early January surface hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new slab avalanches had been reported at the time of publishing</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche have been reported as of publishing Monday evening.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We've receive reports of several natural and skier triggered avalanches ranging from size 1-2 from across the region.&nbsp; It sounds like the surface hoar is starting to wake up!</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported for several days; however, observations are very limited. </span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Size 1.5 storm slabs will likely be reactive to the weight of a person in lee and cross loaded terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches observed - expect sluffing of the recrystallized facets in the upper snowpack to react to ski traffic.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">The current storm system may spark a round of storm slab activity at the highest elevations if the new snow is relatively dry. If the freezing levels stay as high as currently forecast and the mountain tops get mainly rain or wet snow, wet sluffing or wet slab avalanches may occur at all elevations. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Sunday or Monday. On Friday and Saturday, skiers triggered a few storm slabs size 1-2 in the Nelson area. A thin storm slab overlying the recently buried surface hoar was the suspected culprit in all of these avalanches. Storm slab avalanches are expected to increase in size and reactivity with the upcoming new snowfall.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, the Avalanche Canada field team was reporting old natural wind slab avalanches in the north of the region which had likely released sometime over the weekend. On Sunday, ski cutting was producing 5-10cm wind slabs on steep rolls below treeline in the south of the region. Explosives control on Saturday triggered a size 1 wind slab in the south of the region. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, 4 natural avalanches up to size 1.5 were reported to have occurred around Fernie during the night but details were limited due to poor visibility. On Monday, ski-cutting produced several size 1 slabs 10-20cm deep in the alpine and at treeline. These were failing on the early-January surface hoar layer. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Small fresh wind slabs are starting to be reactive to skier triggering at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche have been reported as of publishing Tuesday evening.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We've receive reports of several natural and skier triggered avalanches ranging from size 1-2 from across the region. It sounds like the surface hoar could be starting to wake up!</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">No new avalanches have been reported for several days; however, observations are very limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, reports indicated mostly sluffing up to size 1 from steeper terrain features.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday, numerous small, natural and rider triggered wind slab avalanches up to size 1.5 and widespread loose dry sluffing up to size 1 were reported from the region. With new snow forecast, storm slab avalanches will likely become more of a widespread avalanche problem. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">On Monday, several loose dry avalanches up to size 1.5 occurred from steeper terrain features. With forecast snow, storm slab problems are likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches have been reported. With forecast new snow, building storm slabs and loose snow avalanche problems may persist through Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated size 1.0 storm slabs were reactive to the weight of a person in some isolated wind loaded terrain yesterday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There are still occasional loose dry sluffs out of very steep alpine terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity has been reported, but wet loose snow avalanches may have released from steep slopes during the warm and wet conditions Tuesday night.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported as of Wednesday morning. On Friday and Saturday, skiers triggered a few storm slabs size 1-2 in the Nelson area. A thin storm slab overlying the recently buried surface hoar was the suspected culprit in all of these avalanches. Storm slab avalanches are expected to increase in size and reactivity with additional loading from snow and wind.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Preliminary reports from Wednesday morning include a few explosives triggered up to Size 2, but limited results with ski cutting below treeline likely due to insufficient storm snow settlement and cohesion for storm slab conditions in sheltered areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, sled testing in Smith Basin north of Elkford produced whumpfing and shooting cracks on a slope adjacent to a recent sled triggered small wind slab avalanche. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche have been reported since Tuesdays storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches reported. Expect natural storm snow avalanche cycle occurred today. Storm snow may continue to be easy to trigger, and avalanche size may increase with continued storm loading.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some thin wind slab avalanches were reported on Tuesday. I suspect that there was a storm slab avalanche cycle today. Highways observations reported numerous storm slabs up to size 1.0 in the highway corridor.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Storm slab avalanche up to size 3.0 in the Rogers Pass today. Other operations have reported mostly size 1.5 natural avalanches. One report from the southern Monashees of skier remotely triggering a storm slab about 50 cm deep above surface hoar in a cut block at 1600 metres elevation. Numerous avalanches were reported on Tuesday up to size 2.0 but mostly size 1.0-1.5 that were releasing as storm slabs or loose dry avalanches. Expect storm slabs to continue to be easy to trigger on Thursday. Pockets of wind transported snow may be deep and propagate where they are sitting on weak buried crystals and/or old melt-freeze crusts.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday a couple of reports of slab avalanches size 1.0 were reported from alpine elevations. One of these slabs was remotely triggered from six metres away.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">It sounds like the storm snow is starting to be reactive to skier triggering at treeline and in the alpine.&nbsp; We've receive reports of skier accidental avalanches from the area around Whistler and Avalanche control produced numerous small slab avalanches as well as some larger cornice collapses.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We received reports of several natural and skier triggered avalanches ranging from size 1-2 earlier in the week.&nbsp; These avalanche release on the uppermost layer of recently buried surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">It sounds there has been some surprisingly large skier remote and ski cut releases in wind loaded features.&nbsp; These avalanche have apparently been failing on one of the two buried layers of surface hoar we are concerned with.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous size 1 soft slabs with a few size two slabs from large alpine features were easily triggered on Wednesday. These slabs were running fast and far.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday and Thursday include numerous natural avalanches heard and observed up to Size 2 in response to heavy loading from snow and wind, as well as skier and explosive-triggered storm slabs up to Size 2.5. Also of note were several Size 1-1.5 storm slabs remotely triggered by a snow cat.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">West of the divide recent reports include a Size 1.5 skier triggered storm slab avalanche in the southern Elk Valley. But reports indicate no recent activity east of the divide.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Wednesday include numerous explosive and skier controlled 20-50cm storm slab avalanches, which tended to be more touchy on southern aspects due to sun crust bed surface and more pronounced slab formation. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity has been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">There was wide spread avalanche activity on Thursday with numerous natural, explosive controlled, and skier accidental avalanches ranging from size 1-2. These avalanches failed on the layer of surface hoar down 30 to 40cm on all aspects at treeline and in the alpine.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">The majority of the recent avalanche activity has been reported from areas that saw more snow through the last storm. Explosive control produced avalanches up to size 2 failing on the layer of buried surface hoar on Wednesday. In areas where a storm slab has not yet developed the surface snow is sluffing fast and far.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">One wind lip/small cornice remotely failed from 15m away. The failure plain was preserved surface hoar. 2400m, E aspect at Burstall Pass, immediate lee and very unsupported terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">We've receive sporadic reports of natural, explosive, skier remote and skier triggered avalanches ranging from size 1-2 from across the region through the week. Shooting cracks are being observed wherever the recent storm snow is starring to slab up. We haven't had any recent reports of these surface avalanches steeping down to any of the deeper week layers, although the potential for this to happen could still be there.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We had a report from Valemount that in most areas the recent storm snow was mostly unconsolidated, and not reacting as a slab yet. In some areas the storm snow has been pressed into a slab by the winds and is very easy to trigger where it is sitting on a widespread layer of surface hoar. Expect soft storm slabs to continue to be triggered by human activity. We also had a report on Thursday from the Wells Grey area of a skier remotely triggering a size 2.0 slide that was 35 cm deep from 20 metres away. This avalanche was 80 metres wide and released on buried surface hoar in the alpine. This group also reported numerous whumpfs during the day. These reports suggest that there is some variability across the region. I suspect that the south and west of the region may have more storm snow, and the storm snow may have settled into a more cohesive slab in those 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">Avalanche control in the highway corridor resulted in numerous slab avalanches up to size 2.5 on Thursday. Several operations reported storm slab avalanches releasing naturally to size 2.0 on Wednesday. There were also several reports of skier controlled and accidentally triggered avalanches up to size 1.5 that were 20-40 cm deep, most of these were reported to be sliding on buried surface hoar. I suspect that the storm slab avalanche cycle continued on Thursday. Likelihood of triggering is expected to decrease on Friday. If the sun comes out on Friday, there may be a natural avalanche cycle on steep southerly aspects due to the warming from solar radiation.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control in the highway corridor on Thursday resulted in numerous storm slab releases size 2.0-2.5 on various aspects between 900-1300 metres. Storm slab avalanches up to size 3.0 in the Rogers Pass on Wednesday. Several operations reported skier remote avalanches up to size 2.0 and skier controlled or accidental avalanches up to size 1.5 on Wednesday. The storm snow is settling into a cohesive slab that allows for long fracture propagations and remote triggering. I expect that the likelihood of triggering will be reduced on Friday with the forecast cooling, but will then increase again with Saturdays forecast Pacific storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Some small wind slabs size 1.0 were reported on Thursday morning from the north of the region. These wind slabs were the result of recent moderate northwest winds in the alpine, and they were 10-15 cm deep. On Wednesday a skier remotely triggered a wind slab from 30 metres away that was size 1.5 and the crown was 10-20 cm deep. Also on Thursday in the center of the region we had a report of numerous wind slabs skier controlled to size 1.0 on steep unsupported terrain at treeline. Conditions have been reported to be very different from the Selkirk mountains to the west, where much more storm snow has accumulated.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Numerous size 1 soft slabs with a few size two slabs from large alpine features were easily triggered on Wednesday. These slabs were running fast and far.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">1 loose dry was noted today on Tent ridge. Visibility was poor, but it seemed to start near the ridge and propagate for most of the path. Small slabs were undercut as it went, adding to the mass. Sz2, E aspect and ran to top of the runout.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanche activity has been reported.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Thursday include numerous explosive and skier controlled storm slab avalanches up to Size 2, with up to 60cm thick slabs but generally low density. Sun-exposure in some areas also initiated a loose dry natural avalanche cycle with surface sluffs up to Size 2 on steep south facing slopes.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, natural soft slab avalanches were reported up to size 2. This includes one size 2 from a north aspect at treeline and several size 1-1.5 on southerly aspects below treeline. Explosives triggered several more storm slab avalanches up to size 1.5. All these avalanches were reported to be releasing on the early January surface hoar layers. On Thursday, no new slab avalanches were reported but one natural cornice release was observed. This was a size 2 cornice release from a north aspect at 2300m elevation. The cornice entrained loose snow but did not trigger a slab. Natural and human-triggered avalanches are expected to increase in size and reactivity as the storm progresses over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, natural avalanche activity up to size 2 was reported in the Pemberton area on north and east aspects.&nbsp; These were 30cm thick slabs releasing on a layer of surface hoar and facets.&nbsp; Explosives triggered a couple size 1.5 storm slabs in the Whistler area where the storm slab was only 10-20cm thick.&nbsp; Natural and human-triggered avalanches are expected to increase in size and reactivity as the storm progresses over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A skier accidentally triggered a pocket of alpine wind slab size 1.5 on a north aspect that was 20 cm deep and 20 metres wide in the north of the region. Loose dry snow continues to be reported falling naturally from steep terrain up to size 1.0.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A couple of size 2.0 wind slab avalanches were reported on Thursday that occurred in the upper Kispiox area that were 40 cm deep and 40 metres wide from steep alpine northwest aspects. In the north of the region on the border of the Northwest Coastal region we had a report of remotely triggered avalanches up to size 1.5 in the alpine and at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle up to size 2.0 from various aspects was reported on Friday from west of Valemount. We had a report from Valemount on Thursday that in most areas the recent storm snow was mostly unconsolidated, and not reacting as a slab yet. In some areas the storm snow has been pressed into a slab by the winds and is very easy to trigger where it is sitting on a widespread layer of surface hoar. Expect soft storm slabs to continue to be triggered by human activity. We also had a report on Thursday from the Wells Grey area of a skier remotely triggering a size 2.0 slide that was 35 cm deep from 20 metres away. This avalanche was 80 metres wide and released on buried surface hoar in the alpine. This group also reported numerous whumpfs during the day. These reports suggest that there is some variability across the region. I suspect that the south and west of the region may have more storm snow, and the storm snow may have settled into a more cohesive slab in those 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">On Thursday, some small natural avalanches were reported falling out of steep un-skiable terrain northeast of Terrace. North of Stewart one natural avalanche size 3.0 was reported in the alpine on a northwest aspect, and further north and east several remotely triggered avalanches were reported up to size 1.5.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, widespread natural, explosive, and human-triggered avalanches size 2-3 were reported.&nbsp; These slabs varied in thickness from 20 to 50cm and primarily occurred on north and east aspects between 1600 and 2100 elevation. On Wednesday, numerous natural avalanches were observed up to size 2 in response to heavy loading from new snow and wind, as well as skier and explosive-triggered storm slabs up to Size 2.5. Also of note were several Size 1-1.5 storm slabs remotely triggered by a snow cat.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous natural and human triggered avalanches size 1-2 were reported throughout the region on Thursday.&nbsp; A few natural size 2.5 avalanches were also reported on larger terrain features. These avalanches occurred on all aspects and elevations. This trend is expected to continue throughout the weekend as the snow load increases.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Numerous natural and human triggered avalanches size 1-2 were reported throughout the region on Thursday.  A few natural size 2.5 avalanches were also reported on larger terrain features. These avalanches occurred on all aspects and elevations. This trend is expected to continue throughout the weekend as the snow load increases.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, ski cutting produced isolated soft slab and loose dry avalanches to size 1 in the Castle area. On Wednesday, a natural size 1 wind slab was reported from a steep north-facing hanging snowfield in the Crowsnest Pass area. Also reported was a size 1.5 skier-triggered storm slab avalanche from the Elkford area. This occurred on a north aspect at 1950m elevation. The slab was 10cm thick and released on a layer of surface hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Evidence of a widespread natural avalanche cycle from Wednesday has been observed throughout the Whistler corridor. These slabs were generally shallow, but a few propagated VERY wide and ran long, indicating that they most likely released on buried surface hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some loose snow avalanches reported and observed up to 1.5 with skier traffic or from explosive control work.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosive control on Saturday morning produced a few size 1 loose wet avalanches and some 'no results.' Human-triggered loose wet sluffing remains the primary concern for Sunday as rainfall continues.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, three human-triggered avalanches were reported north of Terrace. A ski-cut produced a size 1.5 on a north aspect at 1300m, a skier accidently triggered a size 1 on a NW aspect at 1400m, and a skier remotely triggered a size 1 from 5m away on a NE aspect at 900m. All three were described as storm slabs 25-30cm thick failing on a layer of surface hoar from January 9th. Also reported on Friday were isolated natural avalanches up to size 2 in the alpine and treeline, as well as loose moist avalanches from steep rocky features below treeline. On Thursday, some small natural avalanches were reported falling out of steep un-skiable terrain northeast of Terrace. North of Stewart one natural avalanche size 3.0 was reported in the alpine on a northwest aspect, and further north and east several remotely triggered avalanches were reported up to size 1.5. On Sunday, natural and human-triggered avalanches are expected as storm snow adds to the slab sitting over a layer of weak surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Thursday, ski cutting produced isolated soft slab and loose dry avalanches to size 1 in the Castle area. On Wednesday, a natural size 1 wind slab was reported from a steep north-facing hanging snowfield in the Crowsnest Pass area. Also reported was a size 1.5 skier-triggered storm slab avalanche from the Elkford area. This occurred on a north aspect at 1950m elevation. The slab was 10cm thick and released on a layer of surface hoar. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday and Saturday explosives control triggered storm slab avalanches to size 2 in the Lizard Range. As weaknesses within the recent storm snow settle and gain strength, I would still anticipate human triggered avalanche activity on the deeper early January layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches were reported on Friday.  On Thursday, a couple of size 2 wind slab avalanches were reported from steep northwest aspects in the alpine.  These occurred in the upper Kispiox area and were typically 40cm deep slabs. In the north of the region on the border of the Northwest Coastal region we had a report of remotely triggered avalanches up to size 1.5 in the alpine and at treeline.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Pockets of wind slab to size 1.5 continue to be triggered naturally or under light loads on a variety of aspects in the alpine. Loose dry snow continues to be reported falling naturally from steep terrain up to size 1.5.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, a few natural storm slab avalanches size 2-2.5 were reported from a variety of aspects. These varied in thickness from 15-45cm and were releasing on the early-January surface hoar layer. On Thursday, natural avalanche activity up to size 2 was reported in the Pemberton area on north and east aspects. These were 30cm thick slabs releasing on a layer of surface hoar and facets. Explosives triggered a couple size 1.5 storm slabs in the Whistler area where the storm slab was only 10-20cm thick. Natural and human-triggered avalanches are expected to increase in size and reactivity as the storm progresses over the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous natural and human triggered avalanches size 1-2 were reported throughout the region on Friday. These avalanches occurred primarily below 1800 m, on all aspects. Of note, was a size 2.5 avalanche that was remotely triggered from 50 m away on <br />Saturday. This speaks to the touchy nature of the buried weak layer. This trend is expected to continue throughout the weekend as the snow load increases.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">A natural avalanche cycle up to size 2 from various aspects was reported on Friday from west of Valemount. We had a report from Valemount on Thursday that in most areas the recent storm snow was mostly unconsolidated, and not reacting as a slab yet. In some areas the storm snow has been pressed into a slab by the winds and is very easy to trigger where it is sitting on a widespread layer of surface hoar. Expect soft storm slabs to continue to be triggered by human activity. We also had a report on Thursday from the Wells Grey area of a skier remotely triggering a size 2 avalanche that was 35 cm deep from 20 metres away. This avalanche was 80 metres wide and released on buried surface hoar in the alpine. This group also reported numerous whumpfs during the day. These reports suggest that there is some variability across the region. I suspect that the south and west of the region may have more storm snow, and the storm snow may have settled into a more cohesive slab in those 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">Numerous natural and human triggered avalanches size 1-2 were reported throughout the region on Friday. These avalanches occurred at all elevations and aspects. This trend is expected to continue throughout the weekend as the snow load increases.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, dry sluffing was reported from steep north facing slopes in the alpine and isolated loose wet sluffing was reported from sun exposed slopes below treeline. On Thursday, no new slab avalanches were reported but one natural cornice release was observed. This was a size 2 cornice release from a north aspect at 2300m elevation. The cornice entrained loose snow but did not trigger a slab. Natural and human-triggered avalanches are expected to increase in size and reactivity as the storm progresses over the weekend and into early next week.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous natural and human triggered avalanches size 1-2.5 were reported throughout the region on Friday. These avalanches occurred at all elevations and aspects. Of note, a size 2.5 avalanche was remotely triggered from 30 m away near Rossland. This trend is expected to continue throughout the weekend as the snow load increases.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">The fresh windslab along ridgelines was very touchy (easily triggered), thin and stiff yesterday. Numerous size 1 soft slabs with a few size two slabs from large alpine features were easily triggered on Wednesday. These slabs were running wide, fast and far.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, numerous size 1 soft slab avalanches were reported in the region. Isolated natural wind slab avalanches were reported from steep leeward features at treeline and in the alpine. These appear to be mainly north through east aspects. Ski-cutting was producing similar results from wind-loaded features at treeline and in the alpine. Slab depths varied from 10 to 40cm thick and many were running on the recently buried mid-January surface hoar layer. On Friday, a few natural storm slab avalanches size 2-2.5 were reported from a variety of aspects. These varied in thickness from 15-45cm and were releasing on the early-January surface hoar layer. Natural and human-triggered avalanches are expected to increase in size and reactivity as the storm continues.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Very little to no significant avalanche activity observed in the forecast region today.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosive control on Saturday morning produced a few size 1 loose wet avalanches and some 'no results.' Human-triggered loose wet sluffing remains the primary concern for Monday as rainfall continues.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, three human triggered avalanches were reported from north of the region. A ski cut on a northwest aspect at 1700m caused sluffing which subsequently triggered a size 1.5 slab avalanche which released on the early-January surface hoar. Two 30cm thick soft slab avalanches were ski cut in a northeast facing cross-loaded gulley feature at treeline. On Friday, dry sluffing was reported from steep north facing slopes in the alpine and isolated loose wet sluffing was reported from sun exposed slopes below treeline. Natural and human-triggered avalanches are expected to increase in size and reactivity as the storm continues.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, numerous explosive-triggered wind slabs size 1-2 were reported north of Stewart.  These were primarily on west through north aspects around 1400m and thicknesses ranged from 10cm to 60cm.  Two of these explosive-triggered avalanches caused sympathetic avalanches to release 70-90m away.  A skier accidental avalanche size 1.5 was also reported near Terrace.  This was a 30cm thick storm slab on a north aspect at 1400m.  Some isolated natural avalanches were also reported from 450m elevation but it is expected that localized large surface hoar near a lake is the culprit.  On Friday, three human-triggered avalanches were reported north of Terrace. A ski-cut produced a size 1.5 on a north aspect at 1300m, a skier accidently triggered a size 1 on a NW aspect at 1400m, and a skier remotely triggered a size 1 from 5m away on a NE aspect at 900m. All three were described as storm slabs 25-30cm thick failing on a layer of surface hoar from January 9th. Also reported on Friday were isolated natural avalanches up to size 2 in the alpine and treeline, as well as loose moist avalanches from steep rocky features below treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, a ski cut produced a size 1.5 wind slab avalanche on a SW aspect at treeline north of New Hazelton. No new avalanches were reported on Friday. On Thursday, a couple of size 2 wind slab avalanches were reported from steep northwest aspects in the alpine. These occurred in the upper Kispiox area and were typically 40cm deep slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend we had limited observations of new avalanches. However, we anticipate continued human triggering of persistent slab avalanches on the surface hoar layer that was buried in early January.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend explosives avalanche control triggered storm and wind slab avalanches to size 2 in the Lizard Range. Forecast strong southwest winds will continue to promote ongoing wind slab avalanche activity with the potential to step down to the deeper early January weak layer.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported, but this may speak to a lack of observations rather than actual conditions. On Sunday natural and human-triggered wind slab avalanches to size 1.5 were reported in the neighbouring Lizard / Flathead and Waterton Regions. I would expect similar conditions in the South Rockies. Continued wind slab activity is expected at higher elevations with new snow and strong southwest winds forecast for Sunday night.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Pockets of wind slab to size 1.5 continue to be triggered naturally or under light loads on a variety of aspects in the alpine. Loose dry snow continues to be reported falling naturally from steep terrain up to size 1.5.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend we had limited observations of new avalanches due to inclement weather. However, there were reports of human triggered avalanches to size 2 below 1800 m. We anticipate continued human triggering of persistent slab avalanches on the surface hoar layer that was buried in early January.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend we had limited observations of new avalanches due to inclement weather. However, there were reports of human triggered avalanches to size 2.5 below 1800 m. </span><span class="s_3FE45715">Of note, a size 2.5 was remotely triggered from 50 m away.</span><span class="s_3FE45715"> We anticipate continued human triggering of persistent slab avalanches on the surface hoar layer that was buried in early January.</span><span class="s_3FE45715" /></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Patterns in avalanche activity seem quite variable across the region. Continued reports from Valemount suggest that the recent storm snow is mostly unconsolidated, and not reacting as a slab yet. In other areas the storm snow is very easy to trigger where it is sitting on a widespread layer of surface hoar. We had a recent report from the Wells Grey area of a skier remotely triggering a size 2 avalanche that was 35 cm deep from 20 metres away. This avalanche was 80 metres wide and released on buried surface hoar in the alpine. This group also reported numerous whumpfs during the day which speaks to the touchy conditions in this area. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">We have been seeing new snow avalanches after each system passes through the area.  You can expect more of the same today.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Nothing new</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Sunday include numerous Size 1-2 storm slab avalanches direct and remotely triggered by skiers on slopes as low-angled as 20 degrees, as well as widespread whumpfing in flatter terrain as low as 1300m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, three human triggered avalanches were reported from north of the region. A ski cut on a northwest aspect at 1700m caused sluffing which subsequently triggered a size 1.5 slab avalanche which released on the early-January surface hoar. Two 30cm thick soft slab avalanches were ski cut in a northeast facing cross-loaded gulley feature at treeline. In the upper Lillooet, numerous recent natural dry loose avalanches up to Size 1.5 were observed below treeline. Subsequent avalanche control produced 25-45cm thick storm slab avalanches up to Size 2, running on the early January surface hoar.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Sunday include several skier, vehicle and explosive triggered 20-60cm thick (or thicker where wind-loaded) slab avalanches up to Size 2. These slabs were both directly and remotely triggered and ran on surface hoar buried on (or around) January 9th at all elevations and on all aspects.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from Sunday include generally small skier triggered storm and wind slabs avalanches, some of which ran on surface hoar buried a week and a half ago. Skier triggered sluffs were also reported to run far.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Avalanche activity has been widespread over the last few days as recent snow has reached a critical load above a volatile weak layer. Human and naturally-triggered avalanches in the size 1-2.5 range have been most prevalent below treeline, but have also occurred at treeline and alpine elevations. Wind slabs have also been reported in wind-exposed terrain. A ski tourer was buried last week, and professionals continue to operate with great caution. Continued human triggering of persistent slab avalanches is likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Numerous size 1-2 slabs were triggered naturally, by skiers and by explosives on Monday. Many of these failed below treeline, on buried surface hoar, about 20-40 cm deep. Wind slabs were also reactive to human triggers in areas affected by recent winds. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Pockets of wind slab and loose dry avalanches to size 1.5 were triggered naturally or under light loads on a variety of aspects in the alpine over the weekend. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Over the weekend we had limited observations of new avalanches. With the forecast static weather pattern I expect a drop in natural avalanche activity; however, human triggered persistent slab avalanches remain a concern in many areas.</span></p>
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</style><p class="p_CC664AAA"><span class="s_71516F31">Initial reports from Monday suggest a very sensitive persistent slab now exists in the Valemount area. A size 2.5 avalanche failed naturally, and skiers triggered wind loaded slopes at around 2100 m, which failed on the buried surface hoar. Skiers also remotely triggered a slab from 50 m away at 1300 m.</span></p><p class="p_CC664AAA"><span class="s_1681A555">In other areas, the persistent slab is also very easy to trigger where it is sitting on a widespread layer of surface hoar. We had a recent report from the Wells Grey area of a skier remotely triggering a size 2 avalanche that was 35 cm deep from 20 m away. This avalanche was 80 m wide and released on buried surface hoar in the alpine. This group also reported numerous whumpfs during the day.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Monday produced slab avalanches to size 2.5. In a few cases, new softer wind slabs stepped down and triggered hard wind slabs which formed over the weekend. These surface and near-surface instabilities may remain sensitive to human triggering over the next few days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been reported, but this may speak to a lack of observations rather than actual conditions. Over the weekend natural and human-triggered wind slab avalanches to size 2 were reported in the neighbouring Lizard/Flathead and Waterton Regions. Similar conditions may have developed in the South Rockies region. Moving forward, natural avalanche activity should taper-off with forecast benign weather; however, wind slabs may remain sensitive to human triggering in higher elevation lee terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Isolated size 1 natural activity has been observed this morning on alpine travel routes. We have been seeing new snow avalanches after each system passes through the area. Cornices have been steadily growing and should be given a wide berth. You can expect more of the same today. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche activity has been pretty limited in the land of 'K' but in Banff/ LLYK National Parks where they have received more storm snow over the January interface and are seeing more skiers triggering loose dry avalanches that are running far and fast and increasingly more dangerous. These avalanches size (1.5-2.0) are now getting big enough to injure and potentially bury someone if the run out was a terrain trap. Skiers need to watch this especially on bigger, steeper, more committing lines in the alpine and ice climbers need to start being more attuned to the changes that are emerging with ice routes that have alpine start zones and in terrain that is in gulley terrain that magnifies the effect of even small avalanches.  The new snow is building up over this weak January 7th interface and now that we have had some wind input, any additional stressors (precipitation, wind, solar inputs) has good potential to tip the scales.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, numerous avalanches were reported in the region. Several natural avalanches were reported including widespread activity up to size 2 north of Stewart and several natural avalanches size 2.5-3.5 north of Terrace. Several skier triggered avalanches were reported which were mostly size 2. This includes a few remotely and sympathetically triggered avalanches which were mostly triggered from 10m away. Explosives also triggered numerous avalanches. The large majority of this avalanche activity released on the Jan 9 surface hoar layer down 30-80cm. The majority of these avalanches were reported on north aspects but there were avalanches on all aspects and elevation bands.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, a small natural cornice release triggered a size 2.5 slab avalanche in the north of the region. Skiers also triggered a few slab avalanches size 1-2 in the north. All these avalanches released on the Jan 9 surface hoar layer down 30cm. Reports from Sunday include generally small skier triggered storm and wind slabs avalanches, some of which ran on the Jan 9 surface hoar. Skier triggered sluffs were also reported to run far on Sunday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Monday, several size 1-1.5 persistent slabs were triggered by skiers directly, or remotely from a distance. These were between 1300 and 2100 m. A size 2.5 avalanche also failed naturally on a NW aspect at 2200 m. Skiers also reported whumpfing and shooting cracks at low elevations. </span></p><p class="p_CC664AAA"><span class="s_1681A555">In many areas, the persistent slab is just a developing problem, while in some spots there is already a deeper or more cohesive slab. We had a recent report from the Wells Grey area of a skier remotely triggering a size 2 avalanche that was 35 cm deep from 20 m away. This avalanche was 80 m wide and released on buried surface hoar in the alpine. This group also reported numerous whumpfs during the day.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">Numerous size 1-2 slabs were triggered naturally, by skiers and by explosives on Monday and Tuesday. Many of these failed at and below treeline, on buried surface hoar, about 20-40 cm deep. A large handful of these were triggered remotely. A couple of larger (size 2.5-3) wind slabs also failed naturally at alpine/ treeline elevations. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Avalanche activity has been widespread over the last few days as recent snow has reached a critical load above a volatile weak layer. Human and naturally-triggered avalanches have been most prevalent below treeline, but have also occurred at higher elevations in some parts of the region. These have mostly been in the size 1-2 range, with many triggered remotely from a distance. Wind slabs have also been reported in wind-exposed terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been observed.</span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Monday, several small slabs were triggered by skiers, including three that were remotely triggered. These were either on wind-loaded features at and above treeline, or in openings at low elevations, where buried surface hoar is largest and most reactive. These events suggest that there is a very touchy interface, but in general there is not enough load above it to create destructive avalanches. This situation could very quickly evolve and become dangerous, so watch for any areas with increased loading from wind or snow, and be alert if temperature changes cause the slab to become more cohesive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In the north of the region on Monday, a few persistent slab avalanches to size 2 were remotely triggered between 1600 and 1700m from a distances of about 5 metres. This demonstrates the sensitive nature of this instability in some areas. A skier also ski cut a size 1 persistent slab avalanche in the Kootenay Pass area. The early January surface hoar was the culprit in all of these events. New snow and wind on Tuesday night may also spark a new round of wind slab activity on Wednesday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, explosives triggered numerous slab avalanches size 1.5-2.&nbsp; Ski-cutting produced a couple size 1 storm slabs on east aspects at 1800m.&nbsp; A skier also remotely triggered a size 1.5 avalanche from 10m away on a NW aspect at 1750m.&nbsp; The majority of the avalanches reported were failing on the early January surface hoar layer down 40-80cm.&nbsp; There are a few more public reported avalanches on the Avalanche Canada Mountain Information Network as well as the South Coast Backcountry Touring facebook page with some great photos that are definitely worth checking out.&nbsp; Reports from Sunday include numerous Size 1-2 storm slab avalanches direct and remotely triggered by skiers on slopes as low-angled as 20 degrees, as well as widespread whumpfing in flatter terrain as low as 1300m.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In the Elk Valley North area on Tuesday, several natural wind slab avalanches to size 1.5 were observed in wind-loaded, high elevation terrain. A size 1 persistent slab avalanche was also noted on a steep cut bank below treeline. New wind and snow on Tuesday night may promote a new round of wind slab activity. In areas where buried persistent weak layers exist, new snow will also add to the likelihood and consequences of triggering the overlying slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control on Monday produced slab avalanches to size 2.5. In a few cases, new softer wind slabs stepped down and triggered hard wind slabs which formed over the weekend. On Tuesday, a skier accidentally triggered a size 2 storm slab near Fernie. The skier lost a ski in the event, but was not buried or injured. New wind and snow on Tuesday night may add new round of wind slab activity. A surface avalanche in motion may also trigger older wind slabs from the weekend or deeper, more destructive persistent slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Monday, explosives triggered several size 1.5-2 slabs which included avalanches running within the storm snow as well as on the early-January weak layer. Natural avalanches were also reported to be releasing below treeline on the early January layer as a result of warming temperatures. On Sunday in the upper Lillooet, numerous recent natural dry loose avalanches up to Size 1.5 were observed below treeline. Subsequent avalanche control produced 25-45cm thick storm slab avalanches up to Size 2, running on the early January surface hoar. On Saturday, three human triggered avalanches were reported from north of the region. A ski cut on a northwest aspect at 1700m caused sluffing which subsequently triggered a size 1.5 slab avalanche which released on the early-January surface hoar. Two 30cm thick soft slab avalanches were ski cut in a northeast facing cross-loaded gulley feature at treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Avalanche control using explosives and ski cutting within the ski area during and after the storm cycle produced size 1-2 soft slab and loose avalanche activity within the storm snow layers. There have been numerous reports of skier and machine triggered avalanches in the backcountry during the past storm cycle up to size 2.0 running on the buried surface hoar layer. The most recent incident occurred yesterday.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed today but conditions were obscured for the better part of the day.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">All signs point to a snowpack that is primed for a large and widespread avalanche cycle with the incoming &quot;Pineapple Express Light&quot; storm arriving on Wednesday night. Reports from the last few days include numerous natural and rider-triggered slabs up to size 2. Many of these were failing on a surface hoar layer down 40-100 cm deep, and most occurred on Northerly aspects near treeline. Many public observers are also noting signs of instability like whumpfing and cracking. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A fairly widespread natural avalanche cycle was reported below treeline on Tuesday. Numerous slab avalanches up to size 2 were observed, primarily on sun affected slopes. On Tuesday there was also an incident on Mount Chief Pascal. One person was partially buried after triggered a 60-80 cm deep slab on North aspect near treeline. Check the Mountain Information Network for photos and more information on this incident. Conditions are primed for a large and widespread natural avalanche cycle with the incoming storm on Thursday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_1681A555">On Monday, several small slabs were triggered by skiers, including three that were remotely triggered. These were either on wind-loaded features at and above treeline, or in openings at low elevations, where buried surface hoar is largest and most reactive. These events suggest that there is a very touchy interface, but in general there is not enough load above it to create destructive avalanches. This situation could very quickly change, so watch for any areas with increased loading from wind or snow, and be alert if temperature changes cause the slab to become more cohesive. On Tuesday, skiers who ventured onto a steep alpine feature in a permanently closed area within a ski area triggered a size 1.5 wind slab. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There is a new report of two skier controlled size 2 slab avalanches from the Ashman area on Tuesday. These failed on the Jan 5/Dec 26 surface hoar layers down 20-50 cm deep. On Monday, a small natural cornice release triggered a size 2.5 slab avalanche in the north of the region. Skiers also triggered a few slab avalanches size 1-2 in the north. All these avalanches released on the Jan 9 surface hoar layer down 30cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Numerous avalanches were reported in the region on Monday and Tuesday. Reports included widespread activity up to size 2 north of Stewart and a natural avalanche cycle up to size 3.5 northwest of Terrace. Several skier triggered avalanches and remotely or sympathetically triggered avalanches up to size 2 were also reported. Most recent avalanches released on the Jan 9 surface hoar layer down 30-80cm. The majority of these avalanches were reported on north aspects, but there were avalanches on all aspects and elevation bands.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Avalanche activity has been widespread over the last few days as recent snow has reached a critical load above a volatile weak layer. Human and naturally-triggered avalanches have been most prevalent below treeline, but have also occurred at higher elevations in some parts of the region. These have mostly been in the size 1-2 range, with many triggered remotely from a distance. Wind slabs have also been reported in wind-exposed terrain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">No new avalanches have been observed. Heavy rain will promoted widespread loose wet avalanche activity in steep terrain at all aspects and elevations.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Numerous large (size 2-3) persistent slabs failed naturally or with human triggers on Tuesday. Many of these were remotely triggered, highlighting the extreme sensitivity of the buried weak layer. This activity has been creeping up in size and frequency over the last few days and now seems fairly widespread, apart from in isolated parts of the region where there is insufficient snow or cohesion for a slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday, a skier accidentally triggered a size 2 storm slab near Fernie. The skier lost a ski in the event, but was not buried or injured. On the same day, numerous size 2 natural storm slabs were also noted in the Lizard Range. On Wednesday, new accumulations were reacting to explosives as a soft storm slab to size 2.5 in high elevation start zones while widespread loose dry avalanches were reported elsewhere. Extreme southwest winds are sure to promote a new round of wind slab activity at all elevations on Thursday. A surface avalanche in motion may also trigger older storm slabs or deeper, more destructive persistent slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Numerous size 1-2 slabs were triggered naturally, by skiers and by explosives on Monday and Tuesday. Many of these failed at and below treeline, on buried surface hoar, about 20-40 cm deep. A large handful of these were triggered remotely, highlighting the volatility of the persistent weak layer. A couple of larger (size 2.5-3) wind slabs also failed naturally at alpine/ treeline elevations. The frequency and size of avalanches are expected to rise over the next couple of days.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In the Elk Valley North area on Tuesday, several natural wind slab avalanches to size 1.5 were observed in wind-loaded, high elevation terrain. A size 1 persistent slab avalanche was also noted on a steep cut bank below treeline. Extreme winds forecast for Thursday will likely spark a new round of wind slab activity. In areas where buried persistent weak layers exist, wind-deposited snow will also add to the likelihood and consequences of triggering the overlying slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In the north of the region, a few recent persistent slab avalanches to size 2 were remotely triggered between 1600 and 1700m from a distances of about 5 metres. This demonstrates the sensitive nature of this instability in some areas. A skier also ski cut a size 1 persistent slab avalanche in the Kootenay Pass area. The early January surface hoar was the culprit in all of these events. New storm loading on Wednesday also produced explosive and human-triggered storm slab activity to size 2.5 on a variety of aspects in higher elevation terrain.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Some size 1.0 natural avalanche activity was observed below tree line this morning. We are expecting a widespread natural avalanche cycle to begin with continued heavy snowfall and rain today as the freezing levels continue to climb towards the mountaintop.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecaster were able to easily trigger a few smaller sz 1 avalanches on wind loaded features at TL in the Burstall Pass area.  These slabs were failing down 20-30cm on the Jan 6th Infterface.  A few sz 1.5 slabs were also observed along ridgelines on N and E aspects in Alpine areas that entrained the loose dry facets on the lower slopes running far.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There is a new report of two skier controlled size 2 slab avalanches from the Ashman area on Tuesday. These failed on the Jan 5/Dec 26 surface hoar layers down 20-50 cm deep. On Monday, a small natural cornice release triggered a size 2.5 slab avalanche in the north of the region. Skiers also triggered a few slab avalanches size 1-2 in the north. All these avalanches released on the Jan 9 surface hoar layer down 30cm. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Explosives control in areas near Bear Pass and northeast of Terrace produced numerous slab avalanches, size 2-3.5, likely failing on the January 9th interface. Some had very impressive propagations. Other areas reported small skier triggered size 1 slabs and some remotely triggered slabs. Thursday's weather may not have been enough to tip off a widespread natural avalanche cycle. Rider triggering and triggering from a distance remain a concern. The size and likelihood of avalanches will be on the rise as the slab continues to develop with more snow, wind, and milder temperatures. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We will have to wait a day or two to determine how extensive the avalanche cycle on Thursday was. My guess is that we saw widespread activity at all elevations with slides up to at least size 3. Natural activity should taper off heading into the weekend. Hopefully the buried surface hoar problems were cleaned out, but I would treat any slope that did not release as being suspect, especially at treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We will have to wait a day or two to determine how extensive the avalanche cycle on Thursday was. My guess is that we saw widespread activity at all elevations with slides up to at least size 3. Natural activity should taper off heading into the weekend. Hopefully the buried surface hoar problems were cleaned out, but I would treat any slope that did not release as being suspect, especially at treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days, storm slab avalanches to size 2.5 were triggered naturally or with explosives in the Lizard range. Several natural size 2 cornice collapses were also noted. Although natural activity may taper-off over the next few days, human triggered wind and storm slabs remain a concern. A surface avalanche in motion may trigger deeper instabilities such as older storm slabs or deeper, more destructive persistent slabs.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Numerous size 1-2 slabs were triggered naturally and by skiers over the last few days. Many of these failed at and below treeline, on buried surface hoar, about 20-40 cm deep. Many of these were triggered remotely, highlighting the volatility of the persistent slab. An increasing number of wind slabs have also been failing at alpine/ treeline elevations, and also running on surface hoar. Forecast rain at low elevations on Friday may lead to wet loose/ wet slab activity, while higher up the mountain, continued storm slab and persistent slab activity is likely.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">On Wednesday, explosives triggered three size 2 wind slabs. On Tuesday, skiers who ventured onto a steep alpine feature in a permanently closed area within a ski area triggered a size 1.5 wind slab.</span></p><p class="p_CC664AAA"><span class="s_A8FEC758">On Monday, several small slabs were triggered by skiers, including three that were remotely triggered. These were either on wind-loaded features at and above treeline, or in openings at low elevations, where buried surface hoar is largest and most reactive. Snow and wind this week could overload the persistent weak layer in some parts of the region.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Recent storm loading promoted explosive and human-triggered storm slab activity to size 2.5 on a variety of aspects in higher elevation terrain. In some cases, avalanches were triggered within the storm snow and then stepped down to the early January surface hoar layer. With forecast snow and wind, storm instabilities are expected to continue. Continued loading will also add mass and sensitivity to the deeper early January persistent weak layer. As the overlying slab gets thicker, avalanches at this interface will become larger and more destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Numerous size 1-2 slabs were triggered naturally, by skiers and by explosives on Monday and Tuesday. Many of these failed at and below treeline, on buried surface hoar, about 20-40 cm deep. A large handful of these were triggered remotely, highlighting the volatility of the persistent weak layer. A couple of larger (size 2.5-3) wind slabs also failed naturally at alpine/ treeline elevations. </span></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Numerous large (size 2-3) persistent slabs failed naturally or with artificial triggers on Tuesday and Wednesday. Many of these were remotely triggered, highlighting the extreme sensitivity of the buried weak layer. These events appear to be on all elevations and aspects, but the distribution of this type of avalanche activity across the entire region is a little uncertain. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days, several natural wind slab avalanches to size 1.5 were observed in high elevation terrain in the Elk Valley North area. A size 1 persistent slab avalanche was also noted on a steep cut bank below treeline. Although observations were limited at the time of publishing this bulletin, extreme winds on Thursday likely sparked a new round of wind slab activity. In areas where buried persistent weak layers exist, wind-deposited snow will also add to the likelihood and consequences of triggering the overlying slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Heavy rain on Thursday likely promoted a widespread loose wet avalanche cycle in steep terrain at all aspects and elevations. Cooling forecast for Friday should limit any further avalanche activity unless cooler temperatures at the end of the storm allow storm slabs to develop near ridgetop. Any lingering storm slab instabilities should strengthen quickly.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Widespread size 1-2.0 avalanche activity occurred below the tree line during the past 24hrs, with a size 1.5 natural observed to have occurred overnight on a NE asp at 1950m in previously controlled terrain. We had limited observations in the alpine yesterday, but isolated ski testing yesterday morning produced size 1.5 activity with widespread propagation. Explosive testing yesterday afternoon for snow cat protection produced two size 2.0 avalanches stopping just short of the cat road. We have had no observations from the backcountry areas during the past 36hrs, although we are expecting a widespread natural avalanche cycle to have occurred.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">No new avalanches were observed on Friday but visibility was limited. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There are very few observations from the region. No new natural avalanches have been reported. One size 1 skier-triggered avalanche was reported on Thursday. This occurred on a relatively small, shallow slope below treeline. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations were very limited during the storm on Thursday; however, it's very likely there was a large and widespread avalanche cycle in most areas. Some observers noted numerous natural and skier controlled slabs and loose wet slides up to size 2. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">We continue to hear reports of small skier-triggered size 1-1.5 slabs and some remotely triggered slabs. Although small, these slabs are occurring on lower angle terrain (25-35 degrees) with surprising propagations. Each day we have received 5-15 cm of new snow. This incremental loading is enough to maintain tricky conditions, but not enough to &quot;clean out&quot; buried persistent weaknesses by causing a widespread avalanche cycle. </span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Tuesday and Wednesday, explosives control in areas near Bear Pass and northeast of Terrace produced numerous slab avalanches, size 2-3.5, likely failing on the January 9th interface. Some had very impressive propagations. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3D0464D1">Numerous size 1-2 slabs were triggered naturally and by skiers over the last few days. Many of these failed at and below treeline, on buried surface hoar, about 20-40 cm deep. Many of these were triggered remotely, highlighting the volatility of the persistent slab. An increasing number of wind slabs have also been failing at alpine/ treeline elevations, and also running on surface hoar. It is likely that a natural avalanche cycle occurred on Friday in response to the warm, windy storm.</span></p><p class="p_CC664AAA"><span class="s_3D0464D1"> </span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Several size 1-2 wind slabs and storm slabs have been triggered naturally and by skiers and explosives this week. Some of these failed on a persistent weak layer of surface hoar or a crust/facet interface. Winds, new snow and rising temperatures increased the size and likelihood of avalanches on Friday. Human triggering remains a real possibility through the weekend.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observations were quite limited during the storm on Thursday; however, a large and widespread avalanche cycle was very likely in most places. In the Coquihalla, a widespread cycle was observed with most avalanches being size 2-2.5 at treeline and in the alpine. At least one size 3 was reported with very impressive propagation. To the north (Upper Lillooet River), a widespread cycle was reported below treeline with avalanches up to size 2.5 being observed. I suspect we will hear more about this cycle in the next day or two. </span></p>
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</style><p class="p_CC664AAA"><span class="s_B8AD0BA7">Numerous size 1-2 slabs were triggered naturally, by skiers and by explosives this week. Many of these failed at and below treeline, on buried surface hoar, about 20-40 cm deep. Many were triggered remotely, highlighting the volatility of the persistent weak layer. A couple of larger (size 2.5-3) wind slabs also failed naturally at alpine/ treeline elevations. It is likely that a natural avalanche cycle occurred on Friday in response to the warm, windy storm.</span><span class="s_3D0464D1" /></p>
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</style><p class="p_CC664AAA"><span class="s_A8FEC758">Numerous large (size 2-3) persistent slabs failed naturally or with artificial triggers this week. Many of these were remotely triggered, highlighting the extreme sensitivity of the buried weak layer. These events appear to be on all elevations and aspects, but seem to have been somewhat limited in distribution across the region. On Friday, a large natural avalanche cycle to size 3.5 was reported by one operator near Valemount. In other parts of the region, the persistent slab may not get such a good clean-out and the problem may linger for human-triggering beyond the end of the storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Heavy rains on Thursday and Friday likely promoted a widespread loose wet avalanche cycle in steep terrain at all aspects and elevations. Cooling forecast for the weekend should limit any further avalanche activity unless cooler temperatures at the end of the storm allow storm slabs to develop near ridgetop. Any lingering storm slab instabilities should strengthen quickly.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from yesterday tell of avalanches up to size 2.5 with explosives, and several skier controlled and skier accidental avalanches up to 1.5 have been reported. In some cases, avalanches were triggered within the storm snow and then stepped down to the early January surface hoar layer. With forecast snow and wind, storm instabilities are expected to continue. Continued loading will also add mass and sensitivity to the deeper early January persistent weak layer. As the overlying slab gets thicker, avalanches at this interface will become larger and more destructive.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days, storm slab avalanches to size 2.5 have been&nbsp; reported, triggered naturally or with explosives. Several natural size 2 cornice collapses were also noted. Although natural activity may taper-off over the next few days, human triggered wind and storm slabs remain a concern. A surface avalanche in motion may trigger deeper instabilities and produce large destructive avalanches.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">In recent days, several natural wind slab avalanches to size 1.5 were observed in high elevation terrain in the Elk Valley North area, as well as east of the divide.&nbsp; A size 1 persistent slab avalanche was also noted on a steep cut bank below treeline. Although observations were limited at the time of publishing this bulletin, strong winds on Thursday and Friday will likely produce a new round of wind slab activity. In areas where buried persistent weak layers exist, wind-deposited snow will also add to the likelihood and consequences of triggering the overlying slab.</span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">There was evidence of widespread natural activity to size 2 yesterday at all elevations.  Limited explosive testing also produced size 2 slabs.  One of these results appeared to have run down to an older layer in the rocks.  </span></p>
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</style><p class="p_CC664AAA"><span class="s_AA239A9B">Forecasters ski cut a sz1 windslab today on a 38 degree, south aspect moraine (known as Mt. Murray Moraines). The avalanche was 10-30cm thick and traveled about 50m. Traditionally, this moraine does not perform with ski cuts so it suggests that windloading is a problem right now.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural slab and loose wet activity up to size 3 was reported on Friday. Activity was observed on all aspects and at all elevations; however, alpine observations were limited due to poor visibility. Cooling temperatures and drier conditions this weekend will help stabilize the snowpack and reduce the likelihood of triggering slab avalanches. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">There are very few observations from the region. A couple natural size 2 slab avalanches were observed in wind-loaded terrain (N-NE aspects) at around 1800 m on Friday. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Observed avalanche activity varies throughout the region. Some reporters observed a fairly widespread avalanche cycle with numerous slabs up to size 2.5, mainly from slopes at and below treeline. Others reported only a couple natural slab avalanches up to size 2 from wind-loaded features. On Friday, there was one report of a size 3.5 slab that was remotely triggered by a helicopter touching down. Variable avalanche activity highlights the current challenges with buried and touchy persistent weaknesses. </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Widespread natural slab and loose wet avalanches up to size 3 were reported throughout the region on Friday. Large slabs were observed on all aspects at all elevations (despite limited alpine observations due to poor visibility). There were also a report of a size 2 accidently skier-triggered slab that sympathetically released several other slabs up to size 2.5 on nearby slopes. Natural activity should slow down with cooler and drier weather this weekend; however, human triggering remains a concern in many areas (especially slopes between 1500 and 1800 m that didn't release naturally during the storm - even low angle slopes). </span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Friday, a large natural avalanche cycle to size 3.5 was reported by one operator near Valemount. Another observer just NW of Blue River reported an impressive natural avalanche cycle at and below treeline with numerous slabs up to 60 cm deep. The story may have been the same for other parts of the region. </span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">A large and widespread natural avalanche cycle was observed on Friday with numerous slab avalanches up to size 3 from all elevations and aspects. Many of these slides were suspected to have failed on the Jan. 4th interface. Natural activity should taper off with cooler and drier weather, but conditions remain primed for human triggering. </span><span class="s_A8FEC758" /></p>
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</style><p class="p_CC664AAA"><span class="s_17AE1194">Numerous  slab avalanches up to size 2.5 have been reported in the past 2 days. Many were naturals as a result of recent storm loading.  A large number were skier controlled. Many of these failed around treeline and below, on buried surface hoar, about 20-40 cm deep. Many of these were triggered remotely, highlighting the volatility of the persistent slab. An increasing number of wind slabs have also been failing at alpine/ treeline elevations, and also running on surface hoar. It is likely that a natural avalanche cycle occurred on Friday in response to the warm, windy storm.</span></p>
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</style><p class="p_CC664AAA"><span class="s_3FE45715">Reports from yesterday include several large ( 2-3) natural avalanches as well as a size 1, loose-wet avalanche below tree line.  Operators are also reporting impressive results with explosives, up to size 2.5.  Precipitation tonight and tomorrow will likely produce a new round of wind slab activity. In places where buried persistent weak layers exist, the likelihood of triggering wind-deposited snow will also increase the chance of affecting the storm slab.  </span></p>