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Avalanche Forecast

Archived

Mar 11th, 2013–Mar 12th, 2013

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

Regions

South Coast.

The avalanche danger will rise throughout the day on Tuesday as snow accumulates, winds increase, and the freezing level rises.

Confidence

Fair - Timing, track, or intensity of incoming weather is uncertain for the entire period

Weather Forecast

Synopsis: A steady southwest flow will drive a series of disturbances onto the south coast this week. There is some uncertainty regarding the timing of each pulse of heavier precipitation, but it’s fairly certain to be a wet and mild week. Overnight and Tuesday: Moderate precipitation – 10-20 cm. The freezing level will rise to around 1500 m by Tuesday afternoon. Winds are strong from the south-southwest. Wednesday: Moderate to locally heavy precipitation – 15-20 cm. The freezing level climbs to 1800 m. Winds remain strong from the south-southwest.  Thursday: Moderate precipitation continues. The freezing level starts near 1600 m but could drop later in the day or by Friday morning.  

Avalanche Summary

Thin wind slabs to size 1.5 were skier triggered on steep north facing slopes on Saturday and Sunday. They were reported to have released on surface hoar buried on March 9th. There was a report of a size 2 skier triggered slab avalanche on a steep southwest apsect in the Steep Creek area (Duffey Lake). This incident happened a few days ago, but highlights the lingering potential for triggering large slab avalanches.

Snowpack Summary

A dusting of new snow overlies a variety of old surfaces which include: a crust at lower elevations and on solar aspects, faceted powder on shaded slopes, and surface hoar. The surface hoar, which was reported from the north of the region, has already been reported to be reactive where it was buried by wind slabs formed by strong southwest winds on Saturday.Between 50 and 80cm below the surface is a layer surface hoar which was buried on February 20th. Triggering this layer has become difficult, but heavy snow or rain this week could be enough new load to awaken this layer in specific areas. Below this the snowpack is generally well settled and strong.

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.