Weather Forecast
A high pressure ridge will continue to bring dry, warm conditions.Friday and Saturday: An inversion will generate an above freezing layer from around 2200 to 3300m. Expect some cloud around 2000 m as well as some strong alpine sunshine. Alpine temperatures will reach around +4C and will feel higher still in the sunshine. Ridgetop winds 20-30 km/h from the NW.Sunday: A cooler day as far as air temperatures go, but cloud dissipating, so treeline areas may actually feel warmer. Slightly windier, with Winds gusting to 30 km/h from the NW.
Avalanche Summary
Minor sluffing up to size 1 was observed in the new snow on Wednesday.
Snowpack Summary
The recent dry, warm weather has generally consolidated the upper snowpack. Old, stubborn hard wind slabs may exist under a skiff of new snow. Steep, sun exposed features are most likely seeing a daily melt-freeze cycle.The biggest concern throughout the region is a layer of weak sugary depth hoar at the base of the snowpack which may coexist with a crust which formed in October. I would continue to be suspicious of any large or unsupported upper elevation slopes, especially if they haven't already avalanched. Possible triggers include a heavy load over a thin spot, a cornice fall or rapid temperature change. Any avalanche failing at this interface would be highly destructive.
Problems
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.