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Avalanche Forecast

Archived

Dec 13th, 2016–Dec 14th, 2016

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

Regions

South Coast Inland.

Beware of wind-loaded and sun-exposed slopes where the recent storm snow has settled into touchy slabs.

Confidence

Moderate - Wind effect is extremely variable

Weather Forecast

Expect continued cold and dry conditions for Wednesday, Thursday and Friday with the chance of some cloud late Thursday into Friday. Winds should remain light and variable for Wednesday and Thursday, but pick up to strong northerlies on Friday. Alpine temperatures are expected to remain in the -10 to -20 range with a weak inversion on Wednesday, but significant cooling for Friday.

Avalanche Summary

No new avalanches have been reported, but expect the recent storm snow to be reactive to light triggers in areas where it has settled into a cohesive slab, such as lee slopes near ridgecrests and terrain breaks and sun-exposed slopes.

Snowpack Summary

30-70 cm of low density snow recently buried the previous variable snow surface, including hard wind pressed or scoured areas, old wind slabs, weak faceted snow, or small surface hoar. Wind slabs that have formed in response to southwest winds during the storm, or subsequent northerly winds, are likely to be touchiest in the south of the region where the most snow fell. Weaknesses have also been found within the recent storm snow with reports of moderate snowpack test results on preserved stellars down 48cm in the Coquihalla Pass area. The widespread mid-November crust typically down around a metre. Recent snowpack tests have shown the crust to be unreactive, but it could become a problem in shallow alpine start zones.

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.