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Avalanche Forecast

Archived

Feb 26th, 2013–Feb 27th, 2013

Alpine
Natural avalanches possible, human triggered probable.
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 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

Glacier.

Weather Forecast

Weak ridge of high pressure will bring cooler temperatures and keep things dry today with some sunny breaks. Next system pushing into the interior tomorrow only bringing light precipitation until Thursday evening when a more significant system arrives.

Snowpack Summary

Top 30 cm settling storm snow. Feb 12 surface hoar and crust layers down 40-55 cm, fist to 1 finger snow over top. Mid pack is well settled.

Avalanche Summary

Avalanche control yesterday west of Rogers Pass summit produced 4 size 3.0 avalanches and 4 size 2.0-2.5.7 natural avalanches size 1.5-2.5 east of the summit.From Feb 24: Skier remote size 2.0, from 30m. 2010m, north aspect,  35-40 degrees. 42 cm deep, 100m X 100m on Feb 12 surface hoar size 3-8

Confidence

Due to the quality of field observations on Tuesday

Problems

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.

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.