{"blocks":[{"key":"64dc1","text":"Continuing snowfall is expected to bring new snow totals to 20-40 cm by Thursday morning. Melt-freeze or rime crust may be found partway within the new snow in some areas, introducing a new likely failure plane and limiting wind transport where it exists. The new snow has formed a storm slab problem above a mix of settling storm snow and windslabs in the upper snowpack after several days of consistent snowfall and southwest wind.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1f27l","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"fd837","text":"Our new snow and another 50-90 cm of recent storm snow will be settling on top of weak, faceted snow that formed during the recent cold snap. As new snow accumulates and temperatures rise, the upper meter of the snowpack may become increasingly upside-down and more likely to avalanche. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":87,"length":8,"key":0},{"offset":245,"length":11,"key":1}],"data":{}},{"key":"bud2j","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6s9jo","text":"We're actively monitoring the early December crust.  In some places, it's down 80 cm, while in wind-loaded terrain features it can be found as deep as 180 cm below the surface. It consists of faceted grains above a bulletproof crust formed by the Atmospheric Rivers of early December. There has been avalanche activity on this crust over the weekend.  Larger avalanches in surface layers as well as natural cornice falls may have potential to step down to this layer in the coming days.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#faceted-snow"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://avalanche.ca/glossary#upside-down-snowpack"}}}}