Avalanche hazard is high. As it decreases over the next few days, conditions will remain very tricky.
Confidence
Fair - Forecast snowfall amounts are uncertain
Weather Forecast
A Pacific frontal system reaches the Interior Tuesday afternoon bringing snow overnight into midday Wednesday. Snow amounts will accumulate anywhere from 10-25 cm with lesser amounts in Northern locations. This will be accompanied by moderate west ridgetop winds, switching NW by the afternoon. Treeline freezing levels will hover around 1000 m. By Thursday an upper ridge will build behind the cold front bringing cooler conditions with mostly cloudy skies and light snow amounts. Friday will see a mix of sun and cloud with flurries and freezing levels at valley bottom.
Avalanche Summary
On Monday, numerous natural and skier triggered avalanches were reported from size 1-2.5 and failing on the buried surface hoar layer 30-60 cm down. In adjacent regions remotely triggered avalanches occurred from distances up to 40 m away, which may exist in certain locations where the surface hoar is more predominant in the Purcells. New snow and wind will add load to the upper snowpack and natural avalanche activity is expected. Best case scenario is the new storm snow will initiate a widespread natural avalanche cycle, however; if it doesn't reach its tipping point then it will likely be primed for rider triggers through the holiday period.
Snowpack Summary
New snow 10-25 cm, accompanied by moderate-strong SW winds will add additional load to the upper snowpack. This brings storm snow totals 40-80 cm above a very touchy surface hoar layer that was buried mid-December. A lower layer of surface hoar is also reactive at the northern end of the range, buried down about 40cm.Below 2100 m this storm slab sits on a thick, solid crust that has been reacting as a perfect sliding layer. Storm slabs will blanket the region and be very touchy to the weight of a skier/ rider, especially in locations that has seen wind effect. A hard rain crust with facets from early November is buried over 1 m down and is still reactive to light loads in some locations.
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.