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Avalanche Forecast

Archived

Dec 31st, 2011–Jan 1st, 2012

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 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

South Columbia.

Confidence

Fair - Freezing levels are uncertain

Weather Forecast

A ridge of high pressure drifts into the area Saturday evening driving overnight temperatures into the mid minus teens. On Sunday morning high clouds steam into the region ahead of the approaching mass of warm air. Light precipitation should begin after lunch, but I'm only expecting 5 or so for the day. The bigger story with the warm front is the rise in freezing levels which could go as high as 2000 m. Winds build to moderate/strong values out of the SW Sunday. A weak cold front affects the area Monday afternoon bringing another shot of light precipitation & lowering temps/freezing levels.

Avalanche Summary

Many small natural avalanches confined to the new snow have been reported from the region. While important to note, the big story is the continued activity on the mid December surface hoar/facet/crust layer. The bottom line is that this layer continues to be very sensitive to skiers & sledders. There are numerous reports coming in of remote triggering, that is, people triggering avalanches from far away. It's also significant that avalanches failing on this layer are being reported in areas we sometimes deem as "safe." Both natural and human triggered avalanches continue to be in issue on treed slopes.

Snowpack Summary

Around 100cm of total storm snow has fallen in the region since Christmas. Winds have redistributed the storm snow into wind slabs that are quite widespread; you can find them at and above treeline in wind exposed locations. Even open areas below treeline are suspect for wind affected snow. A surface hoar/facet/crust interface (persistent weakness aka PWL) from mid-December is buried anywhere from 80-100cm deep & has been quite reactive making for touchy avalanche conditions. Below this lies a well consolidated and strong lower snowpack.

Problems

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.

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.