Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Feb 16th, 2013–Feb 17th, 2013

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

Kananaskis.

Up to 10cm of new snow with light winds expected Sunday. This should do little to change the current danger rating, but keep an eye on localized conditions, especially if the winds are stronger than forecasted.

Confidence

Fair - Timing, track, or intensity of incoming weather is uncertain

Weather Forecast

Up to 10cm of new snow is expected through the day on sunday. Winds will decrease in speed to the light range out of the NW. Alpine temperatures around -12 on Sunday. Monday should bring a clearing trend with colder temperatures and light winds.

Avalanche Summary

Nothing new but visibility was limited.

Snowpack Summary

Soft slab formation continues in the alpine and open areas at treeline due to continued winds and light snowfalls. Slabs up to 70cm thick are present in lee and cross-loaded terrain. Some cornice formation has also occurred. At lower altitudes the snowpack remains weak and facetted.

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.