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Avalanche Forecast

Archived

Feb 6th, 2013–Feb 7th, 2013

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

Regions

South Rockies.

Confidence

Fair - Due to limited field observations

Weather Forecast

Thursday: Trace amounts of new snow / Light west winds / Freezing level at 1200mFriday: Clearing throughout the day / Light northwest winds / Freezing level at surfaceSaturday: Mainly clear skies / Light north winds / Freezing level at surface

Avalanche Summary

No recent avalanches have been reported.

Snowpack Summary

Generally light accumulations overlie a variety of surfaces which include: wind slab at higher elevations, settled storm snow or spotty surface hoar in more sheltered terrain, and a crust on previously sun-exposed slopes. A variable interface buried on Jan 23 is down about 20-40cm. In most locations it appears to be well bonded; however, buried surface hoar (up to 20mm) has been found in isolated  parts of the North Elk valley. This will be something to watch as the overlying slab develops. The lower snowpack is generally well-settled.

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.