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Avalanche Forecast

Archived

Nov 24th, 2015–Nov 25th, 2015

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.
Below Treeline
Natural avalanches unlikely.

Regions

Kananaskis.

Look to sheltered areas at lower elevations for good turns. Wind slabs are widespread at upper elevations. Use caution in shallow snowpack areas where triggering of the wind slabs is more likely.

Confidence

Good

Weather Forecast

Cool air will move into the region for a couple of days bringing cold temperatures and light northerly winds. No precipitation is expected for at least the next few days. A warming trend is expected to push into the area sometime on Friday.

Avalanche Summary

No new avalanches were observed or reported.

Snowpack Summary

Between 5 and 10cm of new snow has fallen in the last 24hrs with light to moderate ridge-top winds. This additional snow has had very little impact on the snowpack. Previously formed wind slabs are widespread through Alpine terrain and open areas at Treeline. Expect to find dense wind slabs in all lee and cross-loaded features, except in sheltered areas at lower elevations.

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.