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Avalanche Forecast

Archived

Dec 17th, 2016–Dec 18th, 2016

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Kootenay Boundary.

Fresh wind slabs are building in unusual places. Use caution as you transition into exposed terrain.

Confidence

Moderate - Intensity of incoming weather systems is uncertain on Monday

Weather Forecast

Sunday: Cloudy with scattered flurries / Light to moderate southwest wind / Alpine temperature -11Monday: Periods of snow: accumulations 15-20cm / Light to moderate southwest wind / Alpine temperature -9 Tuesday: Cloudy with flurries / Moderate to strong wind / Alpine temperature of -7

Avalanche Summary

Recent reports indicate avalanche activity as thin windslabs in the alpine to size 1 and loose now sluffing in steep terrain to size 1.

Snowpack Summary

Around 30cm of faceted powder overlies the facets and surface hoar that was buried last weekend. Variable light to moderate winds have loaded immediate leeward features with touchy wind slabs. A widespread crust that was buried in November is typically down 80-100cm. Recent tests show this persistent weakness has the propensity to propagate large avalanches if triggered, from thin rocky areas, for instance.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.