{"blocks":[{"key":"96s51","text":"10-20 cm of new snow falls over wind affected surfaces and/or a crust.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"50fu9","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"5731j","text":"The south, having endured warmer temperatures and more rainfall, is largely below threshold for avalanches at most elevations. Previous snow has seen extensive wind effect, scouring the rain crust clean in some areas, while piling up to 40 cm over it in others.","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":9,"style":"BOLD"},{"offset":0,"length":10,"style":"UNDERLINE"}],"entityRanges":[],"data":{}},{"key":"1foie","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"doa97","text":"In the north, the new snow may be sitting over a layer of surface hoar crystals, older wind affected snow in the alpine, a thick crust below 1800 m or a combination of these.","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":12,"style":"BOLD"},{"offset":0,"length":12,"style":"UNDERLINE"}],"entityRanges":[{"offset":58,"length":12,"key":0}],"data":{}},{"key":"d3vhv","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"61pgq","text":"A couple of buried weak layers produced large avalanches during a previous storm. Snowpack models and observations in the neighboring Sea to Sky region indicate that these layers have been reset by previous rain at treeline, but uncertainty remains around their status in the alpine. These include a layer of surface hoar down an estimated 90-120 cm and deeper crust/facet combo layer.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"ald5i","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"a5l63","text":"Average snowpack depths in the alpine are now likely closer to 150-200 cm. Below treeline, depths of 30-50 cm have been reported around 500 m, decreasing dramatically with elevation, and still below threshold for avalanches in many areas.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#surface-hoar"}}}}