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Avalanche Forecast

Archived

Dec 15th, 2025–Dec 16th, 2025

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

North Columbia, South Columbia, Glacier, Esplanade, Jordan, North Selkirk, Crawford, Dogtooth, St. Mary, West Purcell, Badshot-Battle, Central Selkirk, Goat, Gold, Kokanee, Retallack, Valhalla, Whatshan.

The snowpack remains ripe for human triggering, with natural avalanches likely where snowfall and strong winds persist.

Avoid exposure to avalanche terrain.

Confidence

High

Avalanche Summary

As of Monday morning, an ongoing avalanche cycle is occuring from heavy snow, wind and rain. Avalanches are expected to fail on mid storm layers and buried weak layers, producing large avalanches as seen in the last storm cycle.

On Tuesday, we expect natural activity may be tapering off, but human triggering remains very likely.

Snowpack Summary

By Tuesday afternoon, storm totals are expected to reach 40 to 85 cm. This adds to the 50-150 cm of rapidly settling snow from last week. Upper elevations are likely heavily wind affected, while treeline and below likely holds a surface crust from recent rain.

Reactive weak layers exist in the mid and lower snowpack, producing avalanches during the last 10 days of heavy snowfall.

  • Surface hoar or facets sit below the recent storm snow.

  • A crust from mid November sits 100-180 cm deep, with faceted snow above.

Weather Summary

Monday Night
Mostly cloudy. Up to 30 cm overnight for the north and east of the region. 3 to 10 cm of snow elsewhere. 50 km/h southwest ridgetop wind. Treeline temperature -3 °C. Freezing level 1700 m.

Tuesday
Mostly cloudy. 2 to 5 cm of snow. 30 km/h southwest ridgetop wind. Treeline temperature -6 °C. Freezing level 1300 m.

Wednesday
Mostly cloudy. 20 to 30 cm of snow. 40 km/h southwest ridgetop wind. Treeline temperature -4 °C. Freezing level 1400 m.

Thursday
Mostly cloudy. 4 to 10 cm of snow. 30 km/h southwest ridgetop wind. Treeline temperature -7 °C. Freezing level 300 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid avalanche terrain during periods of heavy loading from new snow, wind, or rain.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Avoid shallow snowpack areas, rocky outcrops, and steep terrain where triggering is most likely.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.