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Avalanche Forecast

Archived

Jan 4th, 2014–Jan 5th, 2014

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

Regions

Northwest Inland.

Confidence

Fair - Freezing levels are uncertain

Weather Forecast

Sunday: Partly cloudy with sunny breaks. Warm air in the alpine, above freezing to about 2000 metres. Strong Southwest winds.Monday: Strong Southwest winds becoming moderate Westerly. Warm air is expected to remain in the alpine with freezing levels around 1700 metres.Tuesday: Mostly cloudy with light Southwest winds and seasonal alpine temperatures.

Avalanche Summary

No new avalanches reported.

Snowpack Summary

Weaknesses within and under the recent storm snow will likely take several days to settle and strengthen after the storm passes. A number of rain crusts may exist in the upper and mid snowpack, primarily below 1500 m. Deeper in the snowpack a layer of facets/surface hoar formed in early December may be found in the top 100cm. The mid and lower snowpack is still structurally weak and faceted with depth hoar and an early season crust 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.

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.