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Avalanche Forecast

Archived

Feb 8th, 2026–Feb 9th, 2026

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

South Coast, Powell River, North Shore, Sasquatch, Sky Pilot, Tetrahedron.

Higher elevations may hold dry, wind affected snow - watch for wind slabs near ridgelines.

Confidence

Moderate

  • We are uncertain about alpine conditions due to limited field observations.

Avalanche Summary

No new avalanches have been reported, however a small natural cycle may have taken place at higher elevations with new snow/wind/rain.

Snowpack Summary

Light snow continues to fall at higher elevations, reaching 10-35 cm total. Rain will likely affect saturated snow/ground at lower elevations.

Average treeline snow depth is 70 to 150 cm. The snowpack tapers rapidly with elevation, especially on sun-facing slopes.

Weather Summary

Sunday Night
Partly cloudy. 1 to 2 mm of precipitation as snow or rain at treeline. 10 km/h south ridgetop wind. Treeline temperature -1 °C. Freezing level 1200 m.

Monday
Cloudy. 10 to 15 cm of snow. 20 km/h southwest ridgetop wind. Treeline temperature -2 °C. Freezing level 900 m.

Tuesday
Mostly cloudy. 25 to 30 cm of snow. 20 km/h southwest ridgetop wind. Treeline temperature -2 °C. Freezing level 1000 m.

Wednesday
Sunny. 10 km/h northwest ridgetop wind. Treeline temperature -1 °C. Freezing level 1200 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.
  • Be careful with wind-loaded pockets, especially near ridge crests and rollovers.

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.