{"blocks":[{"key":"dv31","text":"A dusting of flurries adds to 10-30 cm loose snow over a variety of wind affected surfaces and facets in the alpine and into treeline. Isolated windslabs remain reactive from recent outflow winds. Fresh southerly winds are impacting loose snow, forming thin new windslabs and hiding older, stiffer slabs.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"aqage","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2k4r9","text":"Below 1800m and on solar features at higher elevations, a thin melt-freeze crust is under the new flurries.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3b8d","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"dgn8r","text":"Below the evolving surface, 50-100 cm of settled storm snow sits on a persistent weak layer from late January that consists of facets at upper elevations, surface hoar in sheltered areas, a melt-freeze crust below 1900 m, and a sun crust on south-facing slopes. There could be more than 100 cm on this layer in wind loaded areas. Although this structure is suspect, we have no recent reports of avalanches failing at this interface within the region.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":127,"length":6,"key":0},{"offset":155,"length":12,"key":1}],"data":{}},{"key":"4a6li","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"7h7b0","text":"A crust from early December, currently considered dormant, may be found around 200+ cm deep in the snowpack.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=crust#faceted-snow"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=persistent+weak+layer#surface-hoar"}}}}