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Avalanche Forecast

Archived

Feb 10th, 2025–Feb 11th, 2025

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

Regions

Akamina, Crowsnest North, Crowsnest South, Elkford East.

Seek out areas that have been sheltered from the wind for the lowest avalanche danger and the best riding.

Confidence

Moderate

Avalanche Summary

Small dry loose avalanches were observed in steep terrain on Sunday. No slab avalanches have been reported in a few days.

If you head into the back country consider submitting a MIN post!

Snowpack Summary

Previous strong westerly wind has scoured slopes in the alpine and formed wind slab on east facing terrain.

20 to 40 cm  of faceted snow overlies a weak layer from late January. This layer consists of a crust on sun exposed slopes and a layer of surface hoar on all other aspects.

The mid and lower snowpack is generally well settled.

Weather Summary

day Night

Clear skies. 10 to 20 km/h north ridgetop wind. Treeline temperature -27 °C.

Tuesday

Mostly sunny. 10 to 20 km/h northwest ridgetop wind shifting to 10 to 20 km/h east ridgetop wind. Treeline temperature -20 °C.

Wednesday

Mostly sunny. 10 to 30 km/h west ridgetop wind. Treeline temperature -10 °C, potential for inversion with warmer temperatures in the alpine.

Thursday

Increasing cloud throughout the day with trace amounts of snow. 10 to 20 km/h south ridgetop wind. Treeline temperature -11 °C.

 

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid freshly wind-loaded terrain features.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.

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.