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Avalanche Forecast

Archived

Mar 11th, 2017–Mar 12th, 2017

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

Regions

Northwest Coastal.

Large avalanches will be widespread for the next few days as the coast gets slammed by a hefty storm.

Confidence

High -

Weather Forecast

SATURDAY NIGHT: Storm intensifying with 10-15 cm of snow and 30-50 km/h south winds.SUNDAY: Stormy with about 20 cm of new snow, 60-80 km/h south winds, alpine temperatures climbing to -5 C.MONDAY: Another 20-30 cm of snow, 70-90 km/h southwest winds, alpine temperatures around 0 C and freezing levels climb to 1000 m.TUESDAY: More snow (15-25 cm), 60-80 km/h south winds, alpine temperatures around -2 C and freezing levels drop to 700 m.

Avalanche Summary

On Friday, wind-loading triggered a size 3 persistent slab avalanche on the February facets on southwest slope. Several cornice and ice falls were reported to entrain loose snow, but did not trigger any slabs. One remotely skier triggered avalanche was reported on a small convexity from 50 m away.The incoming storm has all the ingredients for widespread storm slabs. On top of that, it will also trigger large persistent slab avalanches on buried weak layers.

Snowpack Summary

Expect 20-30 cm of fresh snow on Sunday and thicker, stiffer, and more reactive deposits in lee terrain. The new snow will bury older lingering wind slabs formed by recent outflow winds. The load of the new snow will stress a weak interface buried about 50-80 cm deep composed of facets, crust, and surface hoar. This layer has produced avalanches and alarming snowpack test results on a daily basis for the past week. The lower snowpack is strong, with the exception of basal facets in shallow snowpack areas around Bear Pass and Ningunsaw.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.