{"blocks":[{"key":"b0elt","text":"On Saturday, skiers triggered a small and stubborn size 1 wind slab in the immediate lee of a ridge crest. Limited visibility impacted observations, but we suspect touchy wind slabs were found in the alpine and treeline lee feature. Far to the east, a natural storm slab avalanche cycle size 1-2.5 was reported, most observed on southwest and northeast aspects between 1600-2000 m. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8aq1c","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"7frml","text":"Last weekend, several natural and human-triggered wind slab avalanches were reported (up to size 2.5). Reports indicate that recent storm and wind slab avalanches have failed on a faceted interface from mid-January that developed with cold temperature prior to the last heavy snowfall (see an example in this MIN report).","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":92,"length":8,"key":0},{"offset":309,"length":10,"key":1}],"data":{}},{"key":"1po1p","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"5eq4u","text":"There have been reports trickling in over the past month of natural persistent slab avalanches up to size 3 in the Bulkley Valley. These are thought to have been failing on the November crust/facet layer near the ground. The last reported avalanches on this layer were Monday January 13th. Incremental snowfall and mild temperatures have likely promoted a decreasing trend in reactivity for this avalanche problem. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/glossary#sizes-of-avalanches"}},"1":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/mountain-information-network/submissions/5a277e2e-bdc0-4a9e-90c4-4463171b4b11"}}}}