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Avalanche Forecast

Archived

Jan 1st, 2020–Jan 2nd, 2020

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

Regions

Jasper.

Strong westerly winds will continue to strip and load lee slopes through the region over the next few days.

Weather Forecast

The tail end of a Pacific low will continue to bring light precipitation over the next few days. A weak ridge of high pressure is expected on Thursday followed by another low on Friday. 

CAA's Mountain Weather Forecast for more specific details.

Snowpack Summary

Variable amounts of snowfall through the region, burying large surface hoar, present up to 2200m in sheltered areas. SW winds continue to created new wind slabs on lee features at treeline and above. The bottom of the snowpack consists of very pronounced facets, decomposing crusts and depth hoar.

Avalanche Summary

Concerning results from snowpack tests in Southern forecast region around Mount Wilson. Moderate to hard sudden planar results at treeline on the weak basal depth hoar/facet layers.

Confidence

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.