If more snow than forecast arrives during the day on Thursday, avalanche danger may reach HIGH.
Confidence
Fair - Timing, track, or intensity of incoming weather system is uncertain
Weather Forecast
Snow starting overnight or early Thursday morning combined with strong Southwest winds and alpine temperatures near -10. Expect 10-15 cm of snow by early afternoon with continued strong Southerly winds and alpine temperatures around -5. Another 5-10 cm of new snow overnight, and snow continuing during the day on Friday. Strong Southerly winds are forecast to push warm moist air up over the arctic air that has been sitting to the North of the region. This may result in enhanced snowfall for some areas, and an above freezing layer between 1500-2000 metres in other parts of the region. Generally, I think it will be cooler with more snow in the North and East of the region, and warmer with a mix of snow and rain or freezing rain in the Southwest of the region. The storm should continue on Saturday with another pulse (10-15 cm) of warm and moist air pushed by moderate Southwest winds.
Avalanche Summary
There were a couple of natural cornice falls up to size 2.5 over the past few days, and several thin soft slab or loose snow avalanches up to size 1.0. The new storm starting on Thursday is expected to develop a thick storm slab that may release naturally and also may step down to the mid-January persistent weak layer.
Snowpack Summary
Recent snowfalls have developed a new storm slab that is 30-50 cm thick and sits on a variety of old surfaces including crusts, surface hoar, and old wind slabs. Ski penetration has been reported to be about 50 cm in the North of the region. A crust can be found below about 1900m in the north of the region and below 2200m in the south of the region. At higher elevations the new snow covers old wind slabs formed by moderate southwest winds. Several persistent week layers can be found deeper in the snowpack that may be capped by the overlying crust at lower elevations. The mid-January surface hoar is buried between 40 and 80cm down and remains a concern at treeline and above. The mid-December surface hoar layer is now 80 to 140cm below the surface and appears to be slowly gaining strength.
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.
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.