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Avalanche Forecast

Archived

Dec 23rd, 2013–Dec 24th, 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 avalanches possible, human triggered probable.
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 unlikely, human triggered possible.

Regions

Glacier.

Avalanche hazard is on the rise, be prepared to readjust your plan today to more conservative terrain.

Weather Forecast

Pacific frontal system currently over the interior is bringing light to moderate amounts of snow with a rise in temperature. Ridge top winds are forecast to increase throughout the day from the west. Lingering flurries and partial clearing tomorrow. Another system is forecast to arrive on the 25th.

Snowpack Summary

25cm of recent storm snow. Mid-pack is comprised of settling storm snow and more facetted crystals lower down. The December 8 facet/surface hoar interface is down around 65-80cm, and the November 28 layer is now buried down around 90-105cm.

Avalanche Summary

5 loose natural avalanches yesterday in the highway corridor from size 1.5 to 2.0.

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.