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Avalanche Forecast

Archived

Dec 1st, 2013–Dec 2nd, 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 and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

Glacier.

Conditions have changed from last week. Its time to be more conservative in your decision making.

Weather Forecast

Pacific system bringing snow to the interior into tomorrow. Forecast amounts are variable from light to moderate today to light amounts tomorrow. A high pressure ridge is building. It will clear the skies and cool the temperatures for Tuesday.

Snowpack Summary

20cm of new snow is over the November 28 surface hoar layer which had widespread distribution. This surface hoar layer is sitting on sun crust on steep south aspects or facets elsewhere. The November 12 surface hoar layer is down 50 to 110 cm from tree line to the alpine.

Avalanche Summary

No new avalanches observed yesterday.

Confidence

Intensity of incoming weather systems is uncertain

Problems

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.