Purcells

Variable new snow amounts now blanket our wind slab problems. Keep recent wind loading patterns in mind, even if you're traveling through low density new snow.

High -

Friday night: Mainly cloudy with isolated flurries and a trace to 5 cm of new snow. Light variable winds.Saturday: Sunny with cloudy periods. Light east winds. Alpine high temperatures around -22.Sunday: Sunny. Light northeast winds. Alpine high temperatures around -17. Monday: Sunny. Light northeast winds. Alpine high temperatures around -13.

On Wednesday, numerous natural wind slab avalanches up to size 2 and several human triggered size 1-1.5 releases were reported on primarily south aspects at treeline and above. Here is a link to a video of an avalanche that apparently occurred a few days ago in the Purcells. Great footage that illustrates the current wind slab problem in the region.On Saturday there was a report of a skier triggered size 2 persistent slab avalanche 30-50 cm deep on a northeast aspect in the Dogtooth range. This person was seriously injured after being swept over a 30 m cliff and carried by the avalanche for a total of 650 m. Reports of persistent slab avalanches are becoming less frequent which is creating a low likelihood, high consequence scenario in the snowpack that requires discipline and careful terrain selection to manage effectively.

Limited areas of the region received up to 25 cm of new snow on Thursday. This likely overlies sun crust on solar aspects. Below the variable cover of new snow, Recent strong northeasterly ridge-top winds have created wind slabs on lee features at treeline and above. Below this wind affected layer, older buried wind slabs exist on a variety of aspects. These remain a concern for overlying facets (weak, sugary snow), causing them to remain reactive for longer than is typical for a wind slab problem.Lower down there are two layers of surface hoar (weak, feathery crystals) that were buried at the end of January and mid-January. These layers are around 30 to 80 cm deep and are most prominent at lower treeline and below. The surface hoar may sit on a crust on south facing slopes in specific locations, which is a dangerous combination.The base of the snowpack is composed of weak and sugary faceted grains that sit on a crust. This weak layer has produced large and destructive avalanches that are sporadic in nature and difficult to predict. See the Forecasters' Blog here for more information on this problem.