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Avalanche Forecast

Archived

Mar 7th, 2026–Mar 8th, 2026

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

Regions

South Okanagan, Shuswap, North Okanagan.

New snow and wind continue to form fresh, reactive wind slabs in leeward terrain features at upper elevations.

Confidence

Moderate

  • We are uncertain due to a limited number of field observations.

Avalanche Summary

No recent avalanche activity has been reported. However, observations have been limited.

If you are heading into the backcountry, please share any observations with the Mountain Information Network.

Snowpack Summary

10 to 15 cm of new snow falls on moist surfaces at most elevations.

Within the upper snowpack, there may be a few layers up to 50 cm below the surface containing a combination of surface hoar, facets, or crusts. These layers appear to vary in their distribution and have not triggered recent avalanches, but they could become reactive in isolated areas as additional snow accumulates above them.

The remainder of the snowpack is well consolidated and generally stable.

Weather Summary

Saturday Night
Cloudy. 1 mm of precipitation as snow or rain at treeline. 60 km/h west ridgetop wind. Treeline temperature 0 °C. Freezing level 1800 m.

Sunday
Mix of sun and clouds. 10 to 15 cm of snow. 50 km/h west ridgetop wind. Treeline temperature -4 °C. Freezing level 1400 m.

Monday
Mix of sun and clouds. 2 to 4 cm of snow. 30 km/h west ridgetop wind. Treeline temperature -8 °C.

Tuesday
Mix of sun and clouds. 1 cm of snow. 30 km/h southwest ridgetop wind. Treeline temperature -9 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid freshly wind-loaded features, especially near ridge crests, rollovers, and in steep terrain.
  • Wind slabs are most reactive during their formation.

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.