{"blocks":[{"key":"d6sq7","text":"30-60 cm that fell earlier in the week has been blown by moderate to strong winds in exposed treeline and above since then.  Moderate to strong west and southwestern winds created significant ridgetop snow re-distribution onto lee slopes.  Winds are forecast to shift to northwest overnight and into Monday.  Wind slabs will likely remain reactive to human triggers, and are the most reactive during periods of moderate to strong winds.  Cornice development may be found along ridgecrests and deep windslabs on lee slopes. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":226,"length":4,"key":0},{"offset":438,"length":7,"key":1},{"offset":511,"length":10,"key":2}],"data":{}},{"key":"6oep7","text":"Recent snow fell on a variety of old surfaces including a buried melt-freeze crust reported below 1700m and surface hoar reported around treeline.    This Min from Mt. Fernie on Dec 26th found 5-15cm of low density snow above this  recent crust while this Min near Tunnel Creek found it down 20cm.  This MIN from Lodgepole reports this near surface thin crust disappearing above 1800m.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":155,"length":3,"key":3},{"offset":255,"length":4,"key":4},{"offset":304,"length":3,"key":5}],"data":{}},{"key":"ebdq3","text":"Buried 60-130cm one can find a variety of weak layers from early December. This persistent weak layer, with facetted crystals and surface hoar crystals above is starting to gain strength. This MIN from the 27th near Mongolia Bowl reports finding this crust at 60cm with no notable results in their test pits while this MIN form the 26th saw varying results - including a deep hard result on basal layers.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":80,"length":21,"key":6},{"offset":108,"length":17,"key":7},{"offset":130,"length":12,"key":8},{"offset":193,"length":3,"key":9},{"offset":319,"length":3,"key":10}],"data":{}},{"key":"qg7f","text":"Deeper in the snowpack are two hard melt-freeze crusts that formed in November that may have some weak crystals around them. This potential avalanche problem is dormant at this time, however; it remains on our radar. This layer produced very large and destructive avalanches in shallower snowpacks within one of our nearest neighbours in the recent storm, highlighting the need to remain cautious of it in shallow, rocky alpine snowpacks.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=lee#leeward"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=lee#cornices"}},"2":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=leeward#leeward"}},"3":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/39ed90f1-3519-4fea-88bf-f53171e6d54f"}},"4":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/f9fb80d7-367f-4152-a3ff-32b6883969ee"}},"5":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/af541513-fd0a-48f7-a539-fb7165d45bd5"}},"6":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=persistent+weak+laye#persistent-weak-layer"}},"7":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary?q=facet#facetcrust-layer"}},"8":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#surface-hoar"}},"9":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/cf4db174-aa9e-427f-affa-37dcb87b9a49"}},"10":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/e95b7fba-47c9-46e7-ba6f-8452e76ffe01"}}}}