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Avalanche Forecast

Archived

Dec 21st, 2012–Dec 22nd, 2012

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

Regions

South Coast.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Saturday: Light snowfall / Light southeast winds / Freezing level at surfaceSunday: Trace amounts of new snow / Moderate southeast winds / Freezing level at surfaceMonday: Trace amounts of new snow / Light south winds / Freezing level at 700m

Avalanche Summary

In the wake of Wednesday night's storm, reactive storm slabs to size 2 were reported. Some reports suggest that avalanche activity was more specific to wind affected slopes.

Snowpack Summary

The region has seen a daily supply of light to moderate (with some locally heavy) snow accumulations over the past week. In exposed areas, the new snow most likely exists as a windslab.A layer of surface hoar buried on Dec 10 exists at treeline in the Duffey Lake area and may be more widespread.  A bit deeper in the mid snowpack you might find a surface hoar layer from late November; however, tests seem to be showing limited reactivity on this layer. A generally consolidated mid-pack overlies the deeply buried November crust/facet layer which does not seem to have been reactive lately. This layer has not been observed in the Coquihalla area.

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.