{"blocks":[{"key":"4eus3","text":"By Saturday afternoon, 5-15 cm of snow is forecast to accumulate (with up to 20 cm possible along the Coquihalla) as the freezing level drops to valley bottom. Strong winds from the southwest are expected to switch to the northwest and decrease. This will likely create a complex pattern of reactive wind slabs on lee features at upper elevations.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":314,"length":12,"key":0}],"data":{}},{"key":"1vfkm","text":"Earlier in the week, 15-40 cm of snow buried an interface of near surface facets and sun crusts. The surface hoar associated with this interface in other regions reportedly has a more spotty distribution in this region, and it may persist in isolated areas (sheltered open slopes near and above tree line).","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":61,"length":19,"key":1},{"offset":85,"length":10,"key":2},{"offset":101,"length":12,"key":3}],"data":{}},{"key":"31mau","text":"In the north part of the region (ie. Duffey/Hurley/Goldbridge), a deep instability exists at the base of the snowpack. It has not produced recent avalanche activity, with the most recent event on February 17. Rapid warming or heavy loading by new snow/wind/rain events has the potential to re-awaken this layer.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#leeward"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#faceted-snow"}},"2":{"type":"LINK","mutability":"MUTABLE","data":{"href":"https://www.avalanche.ca/glossary#crusts-are-hard-layers-of-snow-usually-created-by-liquid","target":"_self","url":"https://www.avalanche.ca/glossary#crusts-are-hard-layers-of-snow-usually-created-by-liquid"}},"3":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#surface-hoar"}}}}