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Avalanche Forecast

Archived

Jan 21st, 2014–Jan 22nd, 2014

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

Regions

South Coast.

Confidence

Fair

Weather Forecast

Synopsis: The ridge continues to dominate the weather pattern. No snow for the foreseeable future on the South Coast.Wednesday: Freezing Level: 1500m; Precip: Nil; Wind: Light, VariableThursday: Freezing Level: 3200m Precip: Nil Wind: Light, NorthFriday: Freezing Level: 3000m Precip: Nil Wind: Light, NE

Avalanche Summary

No significant avalanche observations from the last three days with the exception of Sunday when a couple of loose avalanches released naturally from extreme SW facing terrain.

Snowpack Summary

Unseasonably warm daytime temperatures have left the snow surface in rough shape. A crust can be found on steep solar aspects to ridge top and on all aspects below 1600m. The crust can break down during the heat of the day when subjected to still air and direct sun. Previous winds have scoured windward slopes and sculpted sastrugi in exposed areas. The upper 30 cm of the snowpack is settling nicely, but two layers of Surface Hoar down around 60 cm continue to give sudden planar shears in test profiles. There are two lower layers of note near the base of the snowpack. A facet/crust combo from late November (down approximately 100-120 cm) is still giving "sudden" results in compression tests and exists at treeline and alpine elevations. Facets and depth hoar still exist at the base of the snowpack, and are especially robust in alpine features where there was a shallow early season snowpack. This problem has been most widely reported from the Duffey Lake and Chilcotin areas.

Problems

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.