Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Dec 7th, 2012–Dec 8th, 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

South Coast.

Confidence

Fair - Due to variable snowpack conditions on Saturday

Weather Forecast

Overnight and Saturday: A ridge of High pressure will build over the North Coast tonight and then move down onto the South Coast during the morning. Light snow is expected to bring a couple of cms to the region during the evening. Moderate Northwesterly winds and cooling temperatures (-12.0 in the alpine) are forecast by morning. Broken skies in the morning, with some sunny periods in the afternoon.Sunday: A warm front is expected to sweep across the coast on Sunday. Expect light to moderate westerly winds combined with moderate precipitation in the West of the region. Further inland only light precipitation is expected. Freezing levels should gradually rise up to about 1200 metres.Monday: Light precipitation and moderate westerly winds combined with freezing levels rising during the day to about 1300 metres.

Avalanche Summary

Explosive control in the Duffey Lake area resulted in avalanches up to size 2.5 that were 30-40 cms deep on Wednesday.

Snowpack Summary

The Coquihalla has a well settled "right side up" snowpack that is about 190 cms deep at 1550 metres elevation. "Right side up" means that the surface layers are light and soft, and then the layers get progressively more dense as you move down through the snowpack. The ski penetration has been reported to be about 40 cms and the foot penetration is very deep at 80 cms. The light snow is causing a lot of sluffing in steeper terrain, but is not reacting as a slab. The November crust has not been found in the Coquihalla, although we don't have any reports from the high alpine. Conditions may be quite different in the North of this region, please email us your observations if you are out in the field. [email protected]

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.