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 4th, 2015–Dec 5th, 2015

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

Regions

South Coast.

There is a great deal of variability in the region. Avalanche Danger is increasing as a series of storms approaches from the southwest.

Confidence

Low - Due to the number and quality of field observations

Weather Forecast

Light snow Friday night resulting in 3-5 cm by Saturday morning combined with moderate southwest winds. 5-10 cm during the day Saturday with strong southerly winds and freezing levels around 1200 metres. 10-20 cm on Sunday with rising freezing levels and strong southwest winds. Storm continuing on Monday.

Avalanche Summary

No new avalanches reported.

Snowpack Summary

There is a great deal of variability in the region. The Duffey Lake area has received the most snow and rain during the recent storms, and it has also had the highest freezing levels. The Coquihalla has a shallower snowpack with slightly cooler temperatures. Storm slabs of varying depths are developing above a mixture of old surfaces left behind after the recent high pressure. We have not had many observations from this region, if you are out in the mountains please submit your observations to the Mountain Information Network.

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.