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Avalanche Forecast

Archived

Dec 8th, 2012–Dec 9th, 2012

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

Regions

Purcells.

Confidence

Fair - Timing of incoming weather is uncertain

Weather Forecast

The Region will be under a cool, windy NW flow through the forecast period.  Light snow amounts expected, with strong NW winds and freezing levels at valley bottom.Sunday: Mainly dry, snow amounts 5-10 cm, ridgetop winds W 20 km/hr switching NW 30-40 km/hr, alpine temps near -7Monday: Trace of new snow, ridgetop winds NW 30-40 km/hr, alpine temps near -8.Tuesday: Light-moderate snow fall amounts, ridgetop winds SW 20 km/hr, alpine temps near -8.

Avalanche Summary

No new avalanche activity reported.

Snowpack Summary

Wind slabs exist in the upper snowpack on north to northeast aspects at treeline and above. Last weeks storm snow and moderate winds have also shaped unseasonably large cornices.Around 80 cm of snow fell over the past week. This loads a surface hoar layer that was buried on November 28th. Although not widespread in the region, releases on this layer may be likely if you have it in your area. A bit deeper (near 100 cm down) another surface hoar layer that developed during mid-November may still exist. Recent testing around the Invermere area has proved this layer to be unreactive. This does not mean its unreactive throughout the region. Its important to dig down in your local riding area, and test these layers before you disregard them. Near the base of the snowpack is the early November crust. Facet sit facets below it, or it may appear as a sandwich of crusts and facets. In some areas it may only now be primed for triggering with recent heavy loading. Observations have been limited; however, deep and destructive slides have been reported on this layer in a neighboring region.

Problems

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

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.