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Avalanche Forecast

Archived

Dec 27th, 2013–Dec 28th, 2013

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

Regions

Jasper.

Some new snow is on the way. This will surely overload deep persistent slab and basal weakness.  Conservative route selection and avoidance of big terrain in the alpine is advised. Have a safe and happy holiday season!

Weather Forecast

Snow and cooling temperatures are expected in the Icefields area.  Localized areas may see up to 20 cms.

Snowpack Summary

No significant precipitation over the last week (1mm in past 72 hours / 5mm past 7 days). Snowpack is generally shallow, weak, with a variably distributed deep persistent slab overlying weak basal layers of depth hoar, crusts, and/or facets. A steady southwest flow has created pockets of windslab in exposed areas at treeline and above.

Avalanche Summary

1 new natural slab avalanche observed today in the alpine on a Southwest aspect - size 2. Likely ran on basal weakness. Numerous natural slab avalanches to size 2.5 observed in the past week, primarily on cross loaded gully features in the alpine.

Confidence

Intensity of incoming weather systems is uncertain

Problems

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.

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.