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Avalanche Forecast

Archived

Dec 12th, 2021–Dec 13th, 2021

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

Regions

South Coast.

Pay attention to conditions that change with exposure to wind. Maintain margins around wind-drifted features, particularly near ridges and roll-overs. 

Confidence

Moderate - Uncertainty is due to the speed, direction, or duration of the wind and its effect on the snowpack. Forecast snowfall amounts are uncertain.

Weather Forecast

A short burst of southeast wind on Monday

Sunday night: Cloudy, 5-15 cm of snow above 500 m, winds shifting to southeast and increasing to moderate, treeline temperatures near -4 C. 

Monday: Cloudy, 5-15 cm of snow above 600 m, moderate southeast winds easing to light, treeline temperatures near -4 C.

Tuesday: Mainly cloudy, light southwest winds, treeline temperatures near -6 C, freezing level around 400 m.

Wednesday: Cloudy, 5-15 cm of snow over 500 m, moderate south winds, treeline temperatures near -4 C.

Avalanche Summary

A natural avalanche cycle occurred in the early morning hours on Saturday. We received a report of several small (size 1) avalanches releasing 20 cm deep in the storm snow in the North Shore Mountains.

Snowpack Summary

Bands of localized precipitation are forecast to bring another 10-30 cm of snow to the mountains by late Monday. A shift in wind direction from the southwest to southeast may form fresh wind slabs in a tricky cross-loading pattern at upper elevations. Pay attention to changing conditions as you move into wind-exposed terrain. It may be possible to trigger wind slabs in lee terrain features, such as down-wind of ridges and roll-overs. 

An impressive storm over the weekend brought 50-90 cm of snow to the mountains. A gradual rise in temperature during the storm formed a thin crust layer that can be found in areas up to 1400 m. An additional 30-60 cm of snow has accumulated above this mid-storm crust layer since temperatures have cooled. Strong southwest winds 

Below the early December crust layers, the snowpack is generally well-settled. With this storm event, a greater number of areas below treeline are meeting threshold snow depths for avalanches. 

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Be aware of highly variable recent wind loading patterns.
  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.

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.