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Avalanche Forecast

Archived

Feb 7th, 2026–Feb 8th, 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

Rossland, South Okanagan, Shuswap, North Okanagan.

New snow and strong winds may form fresh wind slabs on lee slopes at upper elevations.

Confidence

Moderate

  • We are uncertain about forecast precipitation amounts.

Avalanche Summary

Warm temperatures promoted wet loose sluffing and pinwheeling on steep slopes up to size 1 during the warming on Thursday and Friday. No slab avalanches have been reported in the last week.

With new snow and strong wind in the forecast, human-triggering of wind slabs is possible.

Snowpack Summary

5 to 15 cm of snow is overlying a melt-freeze crust of varying thickness. At upper elevations, strong winds have likely blown this snow onto lee slopes, potentially forming reactive new wind slabs.

Below that, 15 to 20 cm of moist snow is sitting over a surface hoar/ crust layer from late January. Avalanches on this layer are considered unlikely at this time.

The mid and lower snowpack is well settled.

Weather Summary

Saturday Night

Mostly cloudy. 4 to 10 cm of snow. 50 km/h southwest ridgetop wind. Treeline temperature -3 °C. Freezing level 1400 m.

Sunday

Mostly sunny. 10 km/h southwest ridgetop wind. Treeline temperature -3 °C. Freezing level 1400 m.

Monday

Mostly sunny. 20 km/h southwest ridgetop wind. Treeline temperature -4 °C.

Tuesday

Mix of sun and clouds. 1 to 2 cm of snow. 30 km/h southwest ridgetop wind. Treeline temperature -6 °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.
  • Use ridges or ribs to avoid areas of wind-loaded snow.
  • Be careful with wind-loaded pockets, especially near ridge crests and rollovers.
  • Seek out sheltered terrain where new snow hasn't been affected by wind.

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.