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Avalanche Forecast

Archived

Feb 1st, 2014–Feb 2nd, 2014

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

Glacier.

Weather Forecast

A ridge of high pressure remains in place over the region for the forecast period. No precipitation is forecast. Over the next three days expect freezing levels to remain at valley bottom with alpine temps below -15 deg C. Ridge top winds are forecast to be light to moderate from the NW. Skies will remain clear today with possible valley cloud.

Snowpack Summary

5cm of snow has buried various surfaces, with moderate winds moving it around. On steep solar aspects it will bond poorly to a suncrust, and elsewhere it will help preserve surface hoar and surface facets. In the alpine it hides hard windslabs and challenging skiing. The mid-pack is well settled and strong, with weaker basal layers.

Avalanche Summary

No new natural avalanches were observed yesterday. Small loose avalanches (sluffs) have been triggered by skiers in steep terrain. Recently, field teams were able to ski-cut thin (5cm) hard slabs in wind affected areas in the alpine.

Confidence

The weather pattern is stable

Problems

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.

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.