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Avalanche Forecast

Archived

Feb 21st, 2013–Feb 22nd, 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 and human triggered avalanches likely.
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 possible, human triggered probable.

Regions

South Columbia.

Confidence

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

Weather Forecast

Friday: Heavy snowfall / Strong to extreme southwest winds / Freezing level at 1000mSaturday: Light snowfall / Moderate northwest winds / Freezing level at 600mSunday: Light snowfall / Light southwest winds / Freezing level at 1000m

Avalanche Summary

Explosives control produced slab avalanches to size 2.5 in the region. The avalanches, which occurred in the alpine or at treeline elevation, were either older wind slabs or persistent slabs that failed on the February 12th interface.I expect a spike in natural avalanche activity with the weather forecast for Friday. Direct action storm slabs and deeper persistent slab avalanches are very likely with this system.

Snowpack Summary

Between 25 and 55cm of snow is sitting on the reactive surface hoar layer that was buried on February 12th. This interface has also shown reactivity on Southerly aspects where a sun crust formed during the period from February 8th-11th. Buried wind slabs may also exist below ridge crests at higher elevations; but have most likely gained some strength. There are older weak layers that are now buried down around 60-80 cms and also at about 110 cms. These layers have been unlikely to trigger by skiers, but they may still be sensitive to large loads like avalanches in motion or cornice fall.Loading from significant wind and snowfall forecast for Friday will very likely create potent storm slab instabilities as well as increased reactivity on the February 12th interface.

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.