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Avalanche Forecast

Archived

Dec 3rd, 2025–Dec 4th, 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, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Banff Yoho Kootenay, Little Yoho, Banff, East Side 93N, Kootenay, Lake Louise, LLSA, Sunshine, West Side 93N, Field.

Wind slabs remain in lee alpine features and isolated treeline pockets. Identify wind-loaded terrain and steer around it.

Confidence

Moderate

Avalanche Summary

No new avalanches were reported on Wednesday. On Tuesday wind slabs up to size 2 were being triggered with explosives at the ski hills.

Snowpack Summary

The previously soft surface snow has been erased with wind in alpine areas, creating windslabs. Some of this wind effect is down into the treeline, but mostly 20-40 cm of soft snow still remains at TL and below. Below ~2300 m, a rain crust exists below the storm snow. The mid- and lower-snowpack is well settled where thicker, and facetting where thin. Tree-line snow depths range from 60-100cm

Weather Summary

West winds will pick up to 40-50 km/h on Thursday, with the potential for a trace of snow, and treeline temperatures steady at -6C.

Friday will be slightly cooler, with diminishing winds.

For more weather forecast details from Environment Canada, click here.

Terrain and Travel Advice

  • Be especially cautious as you transition into wind-affected terrain.

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.