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Avalanche Forecast

Archived

Dec 27th, 2012–Dec 28th, 2012

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

Cariboos.

Confidence

Fair - Wind speed or direction are uncertain on Saturday

Weather Forecast

Friday: Light precipitation and overcast skies, winds moderate from the west and northwest. Alpine temperatures near -11.Saturday: Light precipitation in the early part of the day with partially sunny breaks in the afternoon. Winds will be strong from the northwest. Alpine temperatures will be near -10.Sunday: A weak ridge of high pressure should bring drier conditions with upper level temperatures remaining cool.

Avalanche Summary

There are no recent avalanche observations to report at this time.

Snowpack Summary

The most recent new snow from the weekend and late last week has been redistributed by the wind creating wind slabs in isolated locations. These are sitting on a generally well-settled mid-pack. Deep persistent instabilities (surface hoar and an early November crust, respectively) located in the middle and near the bottom of the snowpack may still be a concern but there's little recent evidence of them being reactive. It is important to know that we have very limited observations for this region. Digging down and making your own observations, especially in thinner snowpack areas, remains a good idea to assist safe slope selection. If you are spending anytime in the backcountry, send us your observations. Every bit is greatly appreciated! Email us at: [email protected]

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.