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Avalanche Forecast

Archived

Jan 17th, 2026–Jan 18th, 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

Rossland, South Okanagan, Shuswap, North Okanagan.

A crust makes for low avalanche danger but rugged travel conditions. Steep sunny aspects may soften in the afternoon.

Confidence

Moderate

  • Confidence is due to a stable weather pattern with little change expected.

Avalanche Summary

No new avalanche observations.

Snowpack Summary

A widespread crust exists on all aspects to mountaintop. This crust may soften during the day.

The mid to lower snowpack contains a few crust/facet layers, including one buried in mid December, now 50 to 80 cm deep. These layers are not a concern under current conditions.

Weather Summary

Saturday Night
Clear skies. 40 km/h northwest ridgetop wind. Treeline temperature 1 °C. Freezing level 3000 m.

Sunday
Sunny. 40 km/h northwest ridgetop wind. Treeline temperature 0 °C. Isothermal to 2500 m.

Monday
Sunny. 30 km/h northwest ridgetop wind. Treeline temperature -1 °C. Above freezing layer 2000 to 3000 m.

Tuesday
Mostly sunny. 40 km/h northwest ridgetop wind. Treeline temperature -2 °C. Freezing level 700 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.
  • Limit exposure to steep, sun exposed slopes, especially when the solar radiation is strong.

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.