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Avalanche Forecast

Archived

Feb 13th, 2025–Feb 14th, 2025

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

East Kakwa, Kakwa, Pine Pass, Tumbler.

The best riding will be in terrain sheltered from the wind where recent snow remains soft.

Confidence

Moderate

Avalanche Summary

No recent avalanche activity has been reported.

If you do head into the backcountry consider submitting a MIN post.

Snowpack Summary

Extensive wind-affected surfaces are found in alpine and exposed treeline terrain. In wind-sheltered terrain, the upper snowpack is largely low-density and faceted. A hard melt-freeze crust from mid-January may exist approximately 50 to 90 cm deep.

The lower snowpack is consolidated and strong

Weather Summary

Thursday Night

Partly cloudy. 30 to 40 km/h east ridgetop wind. Treeline temperature -20 °C.

Friday

Mostly sunny. 20 to 30 km/h east ridgetop wind. Treeline temperature -22 °C.

Saturday

Sunny. 20 to 30 km/h south ridgetop wind. Treeline temperature -18 °C.

Sunday

Sunny. 10 to 20 km/h south ridgetop wind. Treeline temperature -8 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Pay attention to isolated wind affected features in the alpine, as well as cross-loaded features at treeline.
  • Seek out sheltered terrain where new snow hasn't been affected by wind.
  • Avoid slopes that sound hollow or drum-like.
  • Wind slabs are most reactive during their formation.

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.