{"blocks":[{"key":"1b187","text":"Check out our forecaster blog here for the big picture.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":30,"length":4,"key":0}],"data":{}},{"key":"4vt30","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"13n6p","text":"The upper snowpack is variable, depending on exposure to recent strong winds. Some exposed areas may be stripped back to the Nov 30/Dec 1 Crust. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1p2ut","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6uvd0","text":"A change in wind directions means that you may find wind slabs on many aspects, and on both sides of ridges. Late in the week, wind slabs were built by strong winds that were blowing mostly from the southwest. This weekend, the moderate to strong winds are forecast to be from the northwest.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8k00p","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3lkgv","text":"The Nov 30/Dec 1 crust exists up to 2000 m in the southwest of the region, and may only be found up to 1200 m in areas east of Terrace.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"arat3","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"761aa","text":"At higher elevations where this crust is not present, the storm snow overlies old wind slab or wind stripped ridge tops.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"12ju0","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"e7gcr","text":"Treeline snowpack depths are estimated to be around 2-3 m, and a prominent crust can be found near the base of the snowpack.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"djarb","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"4bjgn","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"edg43","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8mgur","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}}],"entityMap":{"0":{"type":"LINK","mutability":"MUTABLE","data":{"url":"https://www.avalanche.ca/blogs/the-river-has-run-dry"}}}}