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Avalanche Forecast

Archived

Feb 11th, 2013–Feb 12th, 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

Kananaskis.

Up to 5cm of new snow expected in the region by late Tuesday. Strong winds are also forecasted. Little change is expected in the danger rating unless more snow falls than is predicted. Travel is currently easy, with variable ski quality.

Confidence

Good

Weather Forecast

Up to 5cm of snow possible over the next 24hrs. Winds will be strong from the NW increasing to extreme by Tuesday afternoon. Alpine temperatures range between -8 and -12.

Avalanche Summary

Nothing new.

Snowpack Summary

Surface hoar and surface facetting in sheltered N aspects below treeline. Between 0 and 20cm of low density overlies a previously formed hard slab. The bond of this recent snow to the hard slab seems good in most areas. Basal facets persist and the snowpack is quite weak 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.