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Avalanche Forecast

Archived

Feb 12th, 2022–Feb 13th, 2022

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

Vancouver Island.

The hazard is likely Low in most places where a strong surface crust exists. However, if you observe the crust breaking down during the heat of the afternoon, assume that wet loose avalanches could still be possible on steep slopes.

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

One more day of very warm and sunny conditions before the ridge breaks down Sunday night. A weak system is forecast to bring light snowfall Monday morning. 

Saturday night: Mostly clear, light NW wind, freezing levels around 3000 m.

Sunday: Increasing cloud cover in the afternoon, moderate SW wind, freezing levels 2500-3000 m. 

Monday: Light snow in the morning, sunny in the afternoon, moderate NW wind, freezing levels 1000-1500 m. 

Tuesday: Mainly sunny, strong NW wind, freezing levels reaching around 2000 m. 

Avalanche Summary

No new avalanches have been reported recently. A few recent MIN posts are showing a widespread, supportive crust and no recent avalanche activity. If you are out in the mountains, please let us know what you are seeing

For Sunday, stability of the snowpack will be tied to the presence or absence of a surface crust. Wet loose avalanches will remain possible on steep, sun-exposed slopes if the surface crust breaks down during the heat of the afternoon. 

Snowpack Summary

A widespread surface crust has now formed at all elevations. This crust still may have the potential to break down on steep sun-exposed slopes during the heat of the afternoon but this is now becoming pretty unlikely after a few days of melt-freeze cycle. 

Below the surface crust, 10-60 cm of moist or wet snow and deteriorating crust layers sit above the thick late-January crust which extends to mountain top elevations on all aspects. The mid and lower snowpack is considered well settled and strong. 

Shallow snow cover at low elevations leaves many hazards like stumps and creeks exposed at or just below the snow surface.

Terrain and Travel

  • Watch for unstable snow on specific terrain features, especially when the snow is moist or wet.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.
  • The more the snow feels like a slurpy, the more likely loose wet avalanches will become.

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.