{"blocks":[{"key":"dffdd","text":"Incremental snowfall with periods of moderate southwest wind is expected to build shallow wind slabs in lee features at upper elevations. Convective flurries have the potential to bring up to 15 cm to favored areas, which will fall on a variety of snow surfaces including hard wind-pressed snow, a melt-freeze crust, or settled powder in sheltered, shaded areas. Additionally, a thin layer of surface hoar may also exist at this interface that could increase the likelihood of triggering wind slabs above.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":393,"length":12,"key":0}],"data":{}},{"key":"8td4m","text":"Deeper in the snowpack, a gradual cooling trend will improve the overall snowpack stability. In shaded, sheltered areas, 20-40 cm of well-settled snow may sit over a layer of small surface hoar crystals buried Feb 25th. A more prominent persistent weak layer from late January is buried 80-150 cm deep and is composed of a combination of surface hoar, crusts, and facets. The past few days of warm weather were likely the final test on these layers. There is some lingering uncertainty about whether this problem remains reactive on isolated upper elevation slopes on solar aspects in thin snowpack areas. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9fcs3","text":"As described in this MIN report, shallow snowpack areas in the east of the region may harbor a faceted basal snowpack. This structure can typically be managed by avoiding shallow rocky areas where the snowpack transitions from thick to thin. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":21,"length":10,"key":1}],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#surface-hoar"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/map?panel=mountain-information-network-submissions/192e788b-6057-47b4-b7e2-9cbffd913042"}}}}