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Avalanche Forecast

Archived

Feb 28th, 2013–Mar 1st, 2013

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 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 is uncertain for the entire period

Weather Forecast

Thursday night: Around 15 cm snow. Strong SW winds. Freezing level around 600 m. Friday: Light snow. Moderate to strong S winds. Freezing level around 700m.Saturday: Light snow. Light winds. Freezing level dropping to valley floor. Sunday: No snow expected. Light winds. Freezing level at sea level.

Avalanche Summary

Natural avalanches to size 2.5 were triggered by wind loading on lee alpine slopes on Wednesday. Skiers also triggered smaller wind slabs at treeline.

Snowpack Summary

Strong SE to NE winds have created widespread new wind slabs at treeline and above. A layer of surface hoar, facets and/or a crust is buried down about 30-60 cm and has become reactive in areas with enough of a slab above. A deeper interface, now buried about 1 m or more deep, still has the potential for step-down triggering. It’s been observed in the Shames backcountry with hard “pops” results in snowpack tests. Large cornices loom as a threat, as they could act as triggers for avalanches on slopes below. Mid and lower snowpack layers are generally well settled and strong. The exception seems to be the Bear Pass area where basal facets are still reported.

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.