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Avalanche Forecast

Archived

Feb 8th, 2013–Feb 9th, 2013

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

Regions

Glacier.

Be aware of soft slabs where the wind has affected the snow over the last week. Watch out for solar induced avalanches if the sun comes out today, especially on thin or rocky steep south aspects.

Weather Forecast

The weather becomes drier over the next few days as a ridge builds over this region. Expect treeline temperatures of -5 for today with a warm-up to -3 on Saturday. Today the freeze line will rise to 700m, and on Saturday it will rise to 1100m. The winds are forecast to be light to moderate from the NW.

Snowpack Summary

Soft slabs have formed in the alpine and treeline from wind transported storm snow.  On solar aspects, these slabs sit on a sun crust (formed on Feb. 3rd). The mid-pack is generally strong, but has become weaker in shallow areas and around trees and rocks.

Avalanche Summary

Avalanche control operations in the park Wednesday produced 30+ avalanches on all aspects.  Most of these involved surface soft slabs, running to end path or  the top of the fans.  Two larger avalanches ran to the highway.  There were no avalanches reported along the TCH yesterday.

Confidence

Timing or intensity of solar radiation is uncertain

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.