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Avalanche Forecast

Archived

Jan 14th, 2020–Jan 15th, 2020

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

Regions

Northwest Coastal.

It is dangerously cold and windy out there right now. Save your toes for the warmer temperatures and new snowfall this weekend.

Confidence

Moderate -

Weather Forecast

Tuesday night: Clear. Strong valley outflows with moderate alpine wind from the northeast. Alpine temperatures around -27 C.

Wednesday: Sunny. Strong approaching extreme valley outflows with moderate alpine wind from the east. Alpine temperatures around -26.

Thursday: Mix of sun and cloud. Moderate southeast winds. Alpine temperatures around -20.

Friday: Mix of sun and cloud. Moderate south to southeast winds. Alpine temperatures around -20.

Avalanche Summary

A natural windslab cycle, size 2-3 was observed Sunday and Monday morning amid reverse loading by strong outflow winds. In an isolated incident, a crown depth of 2 m was observed on a southeast aspect in the alpine. It is suspected to have stepped down to deep persistent layers from mid December. Cornice and serac failures were also observed, as they typically become brittle in the cold.

Looking forward, windslabs will likely become less reactive as they lose cohesion in the cold temperatures. In sheltered areas, unconsolidated snow may be reactive to human triggering as dry loose sluffs.

Snowpack Summary

Extensive wind effect observed at all elevations. North to east aspects in the alpine have been wind scoured, with isolated hard windslab in lees, and notable cornice growth. Not much snow remains for wind transport by the forecast continued outflow. Snow in protected areas is unconsolidated and well preserved by the cold temperatures.

The mid to lower snowpack is generally well consolidated. Layers of note include a crust 1 m deep, found below 1400 m and a couple of layers of surface hoar 1.5 m deep. The previous storm cycle was a good test of these layers, with only an isolated case of suspected step down to one of the surface hoar layers.

Terrain and Travel

  • Keep your guard up at lower elevations. Wind slab formation has been extensive.
  • Be alert to conditions that change with elevation, aspect and exposure to wind.
  • Avoid terrain traps where the consequence of any avalanche could be serious.

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.