Confidence
Fair - Intensity of incoming weather is uncertain on Friday
Weather Forecast
Thursday night: 10-15cm snow. Freezing level 900m.Friday: 5-10cm snow. Freezing level rising briefly to around 1300m near the coast, then falling back to 900m. Strong westerly winds.Saturday: A cool sunny day. Sunday: Dry but mild, with cloudy periods possible.
Avalanche Summary
Highways avalanche control triggered size 3 slabs up to 1m deep. A skier was carried some distance by an avalanche in the Duffey Lake area on Thursday afternoon. I expect avalanche activity to continue, with less naturally-triggered and more human-triggered events occurring over the next couple of days.
Snowpack Summary
Up to 50cm of recent snow has been shifted by southerly winds into wind slabs on lee slopes in the alpine and at treeline.Below the recent storm snow, three weaknesses exist in the upper snowpack. A surface hoar layer formed in early December overlies facets and is down about 60cm. It is giving easy-very easy, sudden collapse results in snowpack tests.A second surface hoar layer buried around Christmas is also giving easy, sudden planar results.A crust which exists to around treeline, buried on December 17th, adds to the complexity of the snowpack.Persistent weaknesses seem to be more of a concern around the Duffey Lake area than in the Cascades (Coquihalla and Allison Pass).The mid and lower snowpack are generally well-settled and strong.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.