Where there is uncertainty in the snowpack, conservative terrain is the answer. Check out today's Forecaster's blog for tips on managing the spatial variability associated with our current persistent slab problem.
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Avalanche Summary
Reports from the past few days include explosives controlled and natural storm snow avalanches to size 2.5 in the alpine and tree line. There have also been a several reports of skier accidental and skier remote (triggered from a distance) avalanches to size 1.5 at and below tree line. Slab avalanche activity can be expected to persist or possibly increase as our recent snow consolidates into a slab above the range of weak surfaces present at the December 15 interface. In areas where new snow has not yet consolidated into a slab, expect continued potential for triggering loose dry avalanches in steep terrain.
Snowpack Summary
Stormy weather over the past week has brought 50-80cm of new snow to the region. The new snow lies over a wide variety of old surfaces, including large surface hoar (weak, feather-like crystals), hard crusts formed by sun or wind, and sugary facets. The bond at this old snow interface becomes critical as the overlying snow gradually consolidates into a slab. The most concerning areas areas will be those that have seen previous surface hoar development, such as sheltered areas at and below tree line and sheltered northerly aspects in the alpine. Additionally, any steep solar aspects where surface hoar may be sitting on sun crust should be considered areas where this weak layer may be more likely to trigger. A crust which was formed by rain in late November is a major feature in the snowpack and is down approximately 90-120cm at tree line elevations. Snowpack tests suggest the snow above is currently bonding well to it. Snowpack depth decreases rapidly below tree line. Look out for early season hazards such as rocks, stumps, and open creeks.