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Avalanche Forecast

Archived

Mar 13th, 2013–Mar 14th, 2013

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 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 possible, human triggered probable.

Regions

South Coast.

Confidence

Fair - Intensity of incoming weather is uncertain on Saturday

Weather Forecast

Thursday:  Continued moist precipitation.  15 -20mm water expected.  Freezing Level: 1800m, lowering throughout the day.  Wind: Moderate to Strong, Southwest.Friday:  Occasional light showers/flurries. 5mm water expected.  Freezing Level 1500m.  Wind Moderate, SW.Saturday:  Another pulse of moisture makes its way inland.  15mm water expected.  Freezing level tops out around 1800m in the afternoon lowering to 1000m Saturday night.  Wind: Light, SW

Avalanche Summary

A widespread natural avalanche cycle to size 2.5 was reported from the Duffey on Wednesday.  The Coquihalla reports several wet naturals from size 1 - 2.5 running to the top of the runouts.  There was a report of a size 2 skier triggered slab avalanche on a steep southwest aspect in the Steep Creek area (Duffey Lake) on March 8th.  Granted, it's a few days old but it highlights the lingering potential for triggering large slab avalanches.

Snowpack Summary

The storm has delivered around 30 cm as of Wednesday afternoon and another 10 - 20 is expected overnight.  This new snow is bonding poorly to the previous snow surface, which includes faceted snow, surface hoar, and/or a crust, but is most concerning where surface hoar is sitting on a crust on previously sun-exposed sheltered treeline slopes. Around a metre below the snow surface is a layer surface hoar buried on February 20th. Although this layer has a history of producing large avalanches, triggering this layer has now become difficult, and would most likely require a very large trigger on a steep, unsupported slope. Below this interface, the snowpack is strong and well settled.

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.