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Avalanche Forecast

Archived

Mar 1st, 2020–Mar 2nd, 2020

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

Regions

Little Yoho.

Strong to Extreme alpine winds Monday will continue to develop the wind slab problem at upper elevations. Limit your exposure to overhead hazards like cornices.

Great skiing in sheltered areas

Weather Forecast

Increased in cloud cover Monday with scattered flurries through the day. Alpine wind values will stay sustained at 70-90 KM/H from the SW. Expect freezing levels to 1500m. We could see an additional 5cm of snow accumulation Monday night.

Snowpack Summary

5-10 cm of new snow with strong SW winds forming new wind slab in the alpine down to tree line. Watch for buried sun crust on steep solar aspects. The Feb 1 rain crust is down 30-60 cm and present below 1900 m. Generally this area has a strong snowpack, with snow depths over 300 cm in the alpine.

Avalanche Summary

Direct observations of several small natural avalanches initiated from strong SW winds were reported Sunday afternoon. Ski hills reported newly formed reactive wind slabs specific to immediate lee.

Confidence

Intensity of incoming weather systems is uncertain

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.