Regions
Banff Yoho Kootenay.
We are surprised by the size of the avalanches that occurred from avalanche control on Sunday and Monday - up to 400m propagations! More avalanche control planned for Tuesday on Mt. Whymper and Simpson - no skiing or climbing in these areas please.
Weather Forecast
Overcast skies with light precipitation for Tuesday, but no measurable accumulation expected. Temperatures will remain cool, ranging from -12 to -18 and expect winds straight out of the west at about 30-40 km/hr in alpine areas. A bit more snow expected for Wednesday.
Snowpack Summary
40cm of storm snow has developed into a touchy storm slab that is very sensitive to triggers at treeline and above. This sits over a supportive mid-pack, with the lower half of the snowpack consisting of weak facets and depth hoar. There is isolated wind effect near ridge crests only; the notable observation is the lack of wind effect.
Avalanche Summary
Avalanche control on Mt. Bosworth today (near Lake O'Hara) resulted in widespread fracture propagations (up to 400m)that released very easily. The ease and speed of the fractures was surprising; most avalanches occurred in the recent storm snow and one size 3 released on the Dec 19 facets. Lots of storm slab avalanches observed in the backcountry.
Confidence
Due to the number of field observations
Problems
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.
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.