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Avalanche Forecast

Archived

Dec 8th, 2013–Dec 9th, 2013

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

Regions

South Coast.

Confidence

Fair - Timing, track, or intensity of incoming weather system is uncertain on Wednesday

Weather Forecast

Monday: Cloudy with sunny periods.  Precipitation: Nill.  Alpine temperature: High -12. Ridge Winds: Moderate northerly. Freezing level at valley bottom.Tuesday: Mainly cloudy.  Precipitation: Nill. Alpine temperature: High -9. Ridge Winds: Light westerlies. Freezing level: 300m.Wednesday: Mainly cloudy.  Precipitation: Flurries. Alpine temperature: High -3. Ridge Winds: Moderate westerlies gusting to strong. Freezing level: 1100m.

Avalanche Summary

No reports of recent avalanche activity.

Snowpack Summary

Snowpack depths vary greatly across the region with 160cm at treeline in the Cascades  but 50 cm along the Duffy.  Terrain below treeline is still mostly below threshold for avalanche activity.Arctic outflow winds have redistributed the snows that fell last week forming wind slabs on S to SW slopes at treeline and in the alpine.  Surface hoar has been growing over the last week in protected locations near tree line while the cold temperatures have driven faceting throughout the snowpack.A few crusts can be found near the ground, especially at higher higher elevations. There haven’t been any reports of avalanches on these layers, but they're worth looking for it if you dig a pit.

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.