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Avalanche Forecast

Archived

Nov 16th, 2013–Nov 17th, 2013

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

Regions

Kananaskis.

Ice climbers beware of gullies and the likelihood of there being loose dry avalanches. Upcoming winds will redistribute the snow, the snowpack may change quickly as a result.

Confidence

Fair - Due to variable weather conditions

Weather Forecast

Flurries overnight with increasing winds (strong range) out of the West. Temps still predicted to fall.

Avalanche Summary

Loose dry avalanches out of very steep, rocky terrain were observed today.

Snowpack Summary

Up to 10cm's of low density snow has fallen. Moderate winds have left most of this new snow available for transport. Storm slabs probably exist near ridgeline in the ALP. These will be sitting on the hard slabs created during the last wind event. The difference in slab density may make for touchy conditions in specific areas.

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.

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.