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 9th, 2021–Feb 10th, 2021

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.

VERY COLD until the weekend with temperatures between -25c and -36c. This might be a good time to stay closer to your vehicle.

Confidence

High -

Weather Forecast

Wednesday, Thursday and Friday: Low of -36c with daytime highs around -25c. Winds will be light to moderate from the NE. If the COLD is not a good enough indicator, then the wind will for sure convince you. Any kind of delay in the backcountry can seriously put you at risk.

Avalanche Summary

Two small avalanches were observed in steep rocky terrain on south aspects and two size 2 cornice releases were observed in the Goat range.

Snowpack Summary

We are looking at about 60cm of settled snow and just over 2m total snow at tree line. The interface with the storm snow is progressively getting stronger but take the time to dig and evaluate this interface before committing to larger features. Some wind effect in the alpine and our usual concerns for lee features and cross loaded gullies.

Terrain and Travel

  • Pay attention to isolated alpine features as well as cross-loaded features at treeline.
  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.

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.