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Avalanche Forecast

Archived

Dec 13th, 2025–Dec 14th, 2025

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

Regions

Coquihalla, Harrison-Fraser, Manning, Skagit.

Wind slabs may form in high-elevation leeward terrain if there is dry snow available to blow.

The snowpack is meager below treeline and travel may be difficult with early season hazards.

Confidence

Moderate

Avalanche Summary

During the storm last Wednesday, a very large size 3 avalanche stepped down to a persistent weak layer near Allison Pass. Several wet loose avalanches also occurred, see photo captions for more details.

Looking forward, as another atmospheric river brings significant precipitation on Sunday night and Monday, we can expect to see more large avalanches occurring.

Monday

Snowpack Summary

Previous heavy rain and high freezing levels formed a widespread crust that extends into the alpine. The snow surface may be wet from rain at lower elevations.

In the alpine, up to 20 cm of recent snow may be forming wind slabs in leeward north through east-facing terrain. Freezing levels are uncertain, but the rain/snow line is expected to be around 1700 m on Sunday.

A crust with facets, formed in early November, is buried between 50 to 100 cm at treeline. This persistent weak layer has caused some recent large avalanches in the region.

Total snowpack depths range from 80 to 140 cm deep at treeline, and diminish rapidly below 1500 m.

Weather Summary

Saturday Night
Mostly cloudy. 2 to 10 mm of rain at treeline. 50 km/h southwest ridgetop wind. Treeline temperature 6 °C. Freezing level 2700 m falling to 2100 m.

Sunday
Cloudy. 2 to 5 mm of precipitation as snow or rain at treeline. 50 km/h southwest ridgetop wind. Treeline temperature 2 °C. Freezing level 2000 m.

Monday
Cloudy. 50 to 75 mm of rain at treeline. 60 km/h southwest ridgetop wind. Treeline temperature 3 °C. Freezing level 2500 m.

Tuesday
Cloudy. 20 to 35 cm of snow at treeline. 50 km/h southwest ridgetop wind. Treeline temperature -1 °C. Freezing level 1500 m.


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.
  • Wind slabs are most reactive during their formation.
  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.

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.