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

Regions

Cariboos.

Confidence

Poor - Due to limited field observations for the entire period

Weather Forecast

Saturday: The effects of a weak ridge of high pressure will be brief. Generally sunny skies for most of the day. No precipitation expected with light northwesterly winds. Alpine temperatures -12 degrees.Sunday: Generally overcast with light amounts of precipitation accompanied by winds from the northwest at 20-30km/h.Alpine temperatures -8 degrees.Monday: A warm front is expected to give a rise in freezing levels to 900m. Light to moderate precipitation along with moderate to strong westerly winds. Alpine temperatures -9.

Avalanche Summary

There are limited recent observations from this region.

Snowpack Summary

Up to 70 cm of new snow has fallen in the past 5 days. Instabilities (surface hoar layer, and a thin sun crust) may exist within or down 50-70 cm. We have very limited information on the extent or sensitivity of these layers, but suspect them to be reactive under the load of the new snow. A second buried surface hoar layer, down about 115 cm, and the early November rain crust (facet-crust combo), over 140cm down in some locations, remain a concern for isolated deep slab avalanches.Average snow depths at treeline seem to be between 150cm and 190cm. Elevations below 1500m are still reported as below threshold.In general, snowpack data is sparse in this region and significant variations likely exist from one drainage to another. Digging down and making your own observations will be critical to safe slope selection. Any observations from the field are welcome at [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.