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Avalanche Forecast

Archived

Jan 28th, 2026–Jan 29th, 2026

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

South Coast Inland, Birkenhead, Duffey, South Chilcotin, Stein, Taseko.

Small wind slabs may form below ridgetops in isolated areas that receive more than 10 cm of new snow.

Confidence

High

  • We have a good understanding of the snowpack structure and confidence in the weather forecast.

Avalanche Summary

No recent avalanches have been reported.

Snowpack Summary

5 to 10 cm snow and strong southwest wind may form small wind slabs at upper elevations. The new snow overlies a persistent weak layer.

At treeline and above, this layer is primarily a hard crust with weak facets above and/or below.

In sheltered treeline locations and below, this layer may be a combination of hard crust and/or surface hoar.

Cornices are reported to be large and looming. Be mindful of them overhead or when travelling on ridge tops.

The mid/lower snowpack is generally well settled and strong.

Snowpack depth ranges between 150 to 250 cm at treeline elevations.

Weather Summary

Wednesday Night
Mostly cloudy. 3 to 10 cm of snow. 50 km/h southwest ridgetop wind. Treeline temperature -4 °C. Freezing level 1300 m.

Thursday
Mostly cloudy. 3 to 5 cm of snow. 50 km/h southwest ridgetop wind. Treeline temperature -3 °C. Freezing level 1600 m.

Friday
Mostly cloudy. 0 to 5 cm of snow. 60 km/h southwest ridgetop wind. Treeline temperature -1 °C. Freezing level 1800 m.

Saturday
Mix of sun and clouds. 40 km/h southwest ridgetop wind. Treeline temperature -2 °C. Freezing level 2100 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for slabs before you commit to it.
  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.

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.