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Avalanche Forecast

Archived

Jan 9th, 2016–Jan 10th, 2016

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Cariboos.

Watch for isolated wind slabs and loose sluffing.

Weather Forecast

A dominant ridge of high pressure brings continued dry weather, a mix of sun and cloud, light northerly winds and cool temperatures. Above about 2000 m, a temperature inversion is expected to raise temps to around -4.For more details check out https://avalanche.ca/weather.

Avalanche Summary

No new avalanches have been reported. A size 1 cornice failed, but did not trigger a slab.

Snowpack Summary

Isolated wind slabs may be lurking behind ridges and ribs. These overlie old surfaces including surface hoar, facets, and possible sun crusts on steep southerly aspects. Cold and dry weather is drying out the upper snowpack (through faceting). In general, the mid and lower snowpack are strong, with weak layers considered dormant for now. Snowpack depths are variable. Shallow snowpack areas may have weak facetted crystals near the ground.

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.