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Avalanche Forecast

Archived

Jan 28th, 2013–Jan 29th, 2013

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

Regions

Kootenay Boundary.

Avalanche danger may be CONSIDERABLE in the Alpine in areas with highest amounts of recent snow, such as Kootenay Pass.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Monday night: Strong NW winds. Alpine temperature near -4. Very light snow.Tuesday: Light N winds. Alpine temperature near -12. Light snow.Wednesday: Strong NW winds. Alpine temperature near -8. Light snow.Thursday: Light W winds. Alpine temperature near -6. Light snow.

Avalanche Summary

Loose dry avalanches and soft slabs to size 1.5 were triggered naturally and by skiers on Sunday. Explosives triggered several size 1-2 slabs on Monday, failing on a buried crust down 20-30 cm.

Snowpack Summary

Around 15-35 cm snow overlies various old surfaces including surface hoar, facets, hard slabs and crusts. The wind has created soft slabs on lee slopes. As incremental snowfalls build up, a cohesive storm slab is developing. Deeper in the pack (about 50-60cm down), a weak interface exhibits mainly hard to no results in snowpack tests, with isolated moderate, sudden results.

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.