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Avalanche Forecast

Archived

Dec 23rd, 2012–Dec 24th, 2012

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

Regions

South Coast.

Confidence

Fair - Intensity of incoming weather is uncertain on Tuesday

Weather Forecast

Monday: Light SW winds. Alpine temperatures around -8. No precipitation.Tuesday: Light to moderate SE winds. Alpine temperature around -7. Light snow late in the day.Wednesday: Light SW winds. Alpine temperature around -8. Light snow.

Avalanche Summary

Small wind slabs and fast running loose dry avalanches were observed on Saturday.

Snowpack Summary

New wind slabs overlie a generally well–settled snowpack. Surface hoar layers in the upper/mid snowpack appear to have gained strength and are now less of a concern. Near the base of the snowpack, a crust/facet layer appears to be inactive. Although unlikely, triggering an avalanche on this layer may be possible from thin snowpack areas or with a very heavy trigger.

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.