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Avalanche Forecast

Archived

Jan 10th, 2014–Jan 11th, 2014

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

Regions

South Coast.

The forecast snow will be a significant test for weak layers buried deep in the snowpack and will likely cause a natural cycle of deep large avalanches.

Confidence

Fair

Weather Forecast

Tonight and Saturday:  Heavy to very heavy snowfall tonight will continue into Saturday /  Strong to extreme southwest winds / Freezing level 1200mSunday: Moderate snowfall in the north of the region, locally heavy precipitation in the south / Strong to extreme southwest winds / Freezing levels between 700 and 1000mMonday:  Cloudy with scattered flurries or rain / Strong to extreme southwest winds / Freezing levels between 1500 and 2000m.

Avalanche Summary

A size 2 deep persistent slab avalanche was reported on Blackcomb Mountain on January 8. This slide was accidentally triggered by a snowcat and released on facets near the ground. Check out Waynn Flann's blog for photos and more information. Two size 2 slab avalanches (human triggered and natural) were observed in Marriott Basin in the Duffey Lake area last weekend. No injuries were reported. The avalanches occurred around 2100m on south-facing terrain. Both were thought to have ran on a crust/facet interface. Check out our Incident Report Database for more details. These incidents highlight the potential for large, full depth avalanches with additional load of heavy snow forecast for the weekend.

Snowpack Summary

Around 20-30 cm of new snow overlies a variety of old surfaces which may include surface hoar in sheltered terrain, wind-pressed snow in exposed areas, or a crust on previously sun-exposed slopes. Recent moderate S-SW winds have produced new wind slabs in exposed lee terrain and cross-loaded features. In the north of the region, recent storm snow is sitting on a weak layer of buried surface hoar which formed in early December. Facets from December's cold snap also seem fairly feature of the snowpack in this part of the region. In some areas, these facets may co-exist with a crust. In shallow snowpack areas, the facets may exist at ground level. These persistent weaknesses will likely wake-up with new snow forecast heading into the weekend.Snowpack depths at treeline range from 140-190 cm in the south of the region, and from 80- 130 cm in the north of the region.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.