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Avalanche Forecast

Archived

Jan 8th, 2026–Jan 9th, 2026

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

Regions

Chic-Choc Mountains, Chic-Chocs.

In the mountains, conditions are stable, snow cover is highly variable, and the danger of wind slabs remains very isolated in alpine terrain.

Confidence

High

  • Confidence is due to a stable weather pattern with little change expected.
  • The snowpack structure is generally well understood.

Snowpack Summary

The surface snow has been heavily affected by westerly winds. In sheltered areas, there is 20 to 30 cm of light snow on the surface. Facets are developing on the December 20 melt freeze crust, which is between 30 and 50 cm deep.

Due to the wind, snow distribution is very uneven in alpine terrain and near treeline: some slopes are almost bare, while others have significant accumulations of wind-blown snow.

The average snow depth at mid-mountain ranges from 60 to 100 cm.

Weather Summary

WEATHER FOR THE CHIC-CHOCS RIDGES AND PEAKS

Thursday evening and night: Cloudy. Northwest wind 12 mph. Low -14.

Friday: Sunny and cloudy. Chance of freezing rain and/or snow up to 2 inches in the evening. South wind 18 to 31 mph. High 32.

Saturday: Snow up to 15 cm. Wind from the west 10 to 50 km/h. Low -13.

Sunday: Snow up to 5 cm. Wind from the east 10 to 50 km/h. Low -10.

For more details, see the Chic-Chocs alpine weather forecast.

Terrain and Travel Advice

  • Watch for areas of hard wind slab on alpine 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.