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Avalanche Forecast

Archived

Jan 1st, 2026–Jan 2nd, 2026

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

Regions

Northwest Coastal, Boundary, Stewart.

Watch for signs of wind loading as you move into more open trees.

Avoid leeward features, where you're still likely to trigger a slab.

Confidence

Moderate

  • Uncertainty is due to the limited number of field observations.

Avalanche Summary

A large avalanche cycle occurred on Tuesday, ending on Wednesday. Numerous large (size 2-3) storm slab avalanches were reported.

No new avalanches have been reported on Thursday.

Snowpack Summary

70-100 cm of snow fell during the recent storm early in the week. Most areas received snow above 1100 m. This new snow fell on a previously wind-affected and faceted surface from the outflow event at the end of December.

Treeline snow depths throughout the region range from 250 cm to 350 cm.

Weather Summary

Thursday Night
Partly cloudy. 10 km/h northwest ridgetop wind. Treeline temperature -11 °C.

Friday
Mostly sunny. Calm winds. Treeline temperature -13 °C.

Saturday
Mix of sun and clouds. 1 cm of snow. 10 km/h south ridgetop wind. Treeline temperature -13 °C.

Sunday
Mix of sun and clouds. 10 km/h south ridgetop wind. Treeline temperature -15 °C.


More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.
  • Carefully evaluate steep lines for wind slabs.

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.