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Avalanche Forecast

Archived

Jan 27th, 2017–Jan 28th, 2017

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

Regions

Jasper.

Wind, snow and warming temperatures may increase the avalanche hazard on Sunday.  Stay tuned!

Weather Forecast

Moderate SW winds can be expected at tree line and above building to strong on Sunday.  Temperatures will be mild with 10 cm possible on Sunday (rain showers in valley bottom).  Expecting clearing, winds easing and temperatures cooling beginning of next week.

Snowpack Summary

The snowpack is unpredictable. Shallow wind slabs have been failing on solar aspects in the alpine.  In sheltered areas, approximately 10-15 cm of settled snow is sitting on a weak and faceted mid-pack with depth hoar to ground.  The November crust  exists sporadically and is hard to find in the southern forecast area.

Avalanche Summary

Large slab avalanches to size 3 have been reported recently on open solar aspects in the alpine.

Confidence

Timing, track, or intensity of incoming weather system is uncertain on Sunday

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.