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Avalanche Forecast

Archived

Dec 26th, 2011–Dec 27th, 2011

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

Sea To Sky.

Confidence

Fair - Timing of incoming weather is uncertain

Weather Forecast

A series of frontal systems will continue to affect the region over the next few days. In general, expect 15-25cm of snow each 12 hour period, with moderate to strong W-SW winds, and fluctuating freezing levels (FL). Tuesday: 30-40cm, heaviest in the evening/overnight. Strong SW winds, rising overnight. FL around 800-1000m gradually rising. Wednesday: 25-40cm, heaviest overnight. Strong W-SW winds. FL rising to 1600-1800m. Thursday: 20-35cm. Strong SW winds. FL lowering to 1000m.

Avalanche Summary

Numerous Size 1-2 slab avalanches have been reported in the past 48 hours, primarily in wind affected terrain near ridge crests. Expect the size and likelihood of avalanches to increase through the forecast period.

Snowpack Summary

The new snow continues to pile up with an additional 15-25cm falling Sunday through Monday afternoon. Touchy wind slabs up to 60cm deep have formed on north through east aspects in response to strong SW winds. A weak rain crust is found below the new snow up to treeline elevations. This crust may sit on top of buried surface hoar and/or facets may persist 10-20cm below. Watch this layer as it gets more load and a thick cohesive slab develops, particularly below treeline where the buried surface hoar would be especially large. A strong mid pack overlies basal facets that have also gained considerable strength. Snow depths are at approximately 150cm at treeline in the Spearhead area and 180cm at treeline in the Brandywine area.

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.