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 16th, 2012–Dec 17th, 2012

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

South Coast.

Danger ratings are set for the Coquihalla, where recent storms have been focussing heavy snow. Conditions in the rest of the region are less touchy.

Confidence

Fair - Due to variable weather conditions

Weather Forecast

Sunday night: Moderate SE winds. 5-10 cm snow (locally up to 30 cm around the Coquihalla). Freezing level at surface.Monday: Strong winds changing from SE to W. Alpine temp lowering to -10. A few cm snow.Tuesday: Light to moderate SE winds. Alpine temp -7. Very light snow. Wednesday: Light SE winds. Alpine temp -11. 20 cm snow.

Avalanche Summary

There were a few reports of small natural and human triggered loose snow avalanches, and isolated thin wind slabs immediately lee of ridge crests late last week. Previous reports include evidence of large avalanches, including one from Mt Joffre at 2000m and the east face of Cayoosh Mountain in the Duffy Lake area last weekend (check out Wayne Flann's Avalanche Blog for a photo of the Cayoosh avalanche).

Snowpack Summary

Deep new snow affected the Coquihalla much more than other parts of the region over the weekend. The next system forecast to arrive overnight Sunday/Monday is likely to follow the same pattern. This means that storm slabs and wind slabs will probably be more widespread around the Coquihalla than elsewhere. New snow may have buried a thin layer of surface hoar in some areas. Moderate westerly winds are likely to have created wind slabs in lee terrain. The late November surface hoar down 70-130 cm produces inconsistent results with snowpack testing. A well settled and rounding mid-pack is overlying the deeply buried November crust/facet layer, which continues to give occasional sudden planar compression test results. This layer has not been observed in the Coquihalla.

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.