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Avalanche Forecast

Archived

Dec 11th, 2013–Dec 12th, 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 possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

South Columbia.

Confidence

Fair - Track of incoming weather systems is uncertain on Thursday

Weather Forecast

Thursday: Moderate to locally heavy snowfall (highest amounts forecast for the Monashees) / Moderate to strong westerly winds / Freezing level at valley bottomFriday: Light snowfall / Moderate northwesterly winds / Freezing level at 1000mSaturday: Moderate snowfall / Moderate southerly winds / Freezing level at 1000m

Avalanche Summary

Numerous low density surface sluffs and soft slabs to size 2 were reported in the region reacting in response to recent storm loading. In recent days a size 2 skier-triggered slab avalanche released on the late-November interface on a north aspect 40 degree slope at 1900m. I would expect ongoing storm instabilities with weather forecast for Thursday.

Snowpack Summary

Moderate to locally heavy amounts of low density snow now overlie generally faceted surfaces that formed during the recent cold snap. At the same buried interface you may find small surface hoar on sheltered slopes or windslabs in exposed terrain. The developing storm slab is likely to become more reactive as slab properties increase with ongoing snowfall, warmer temperatures and wind.Professionals are still keeping their eye on the late-November interface which consists of sun crusts on steep south facing slopes and surface hoar in sheltered areas. Although this layer seems to have become less reactive, it may be triggered on steeper, unsupported terrain or by the weight of the new snow.At the base of the snowpack is a crust/facet combo that formed in October. About 60cm above the ground is a surface hoar layer which formed in early November. These layers have become generally inactive; however, residual risk of large, destructive avalanches exists, especially in areas with a thinner snowpack.

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.