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Avalanche Forecast

Archived

Feb 10th, 2014–Feb 11th, 2014

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

Regions

Northwest Coastal.

Confidence

Fair - Timing, track, or intensity of incoming weather system is uncertain on Tuesday

Weather Forecast

Tuesday: Light snowfall throughout the day becoming heavy through the evening / Strong southwest winds / Freezing level at surfaceWednesday: Steady snowfall in the early morning becoming light / Strong southwest winds / Freezing level at surfaceThursday: Moderate snowfall / Strong southwest winds / Freezing level at 400m

Avalanche Summary

No new avalanches were reported, although observations were limited due to blowing snow.

Snowpack Summary

A developing storm slab overlies a medley of old surfaces which include: weak surface facets, surface hoar, thin wind slabs, a scoured crust, or any combination thereof. Strong winds are likely shifting the new snow into stiff wind slabs in exposed terrain. As the new slab develops and gains cohesion, I would expect it to have a poor bond with any of these old surfaces.The mid and lower snowpack are generally strong and well-settled. Basal facets and depth hoar are likely to exist in some parts of the region, but triggering has become unlikely.

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.