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Avalanche Forecast

Archived

Feb 3rd, 2013–Feb 4th, 2013

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

Regions

Glacier.

Weather Forecast

High pressure ridge exiting the region today. Polar front will bring cooler temperatures with light precipitation overnight and into Monday.

Snowpack Summary

Dense settling recent storm snow in top 40cm. A profile at 2210m, SW aspect, 34 degrees showed 240cm of snow. The Jan 4 crust was down 145cm and the Nov 6 crust was decomposing and 28cm from the ground. One test result in the hard range down 38cm.

Avalanche Summary

4 natural slab avalanches size 2.0 to 2.5 east of Rogers Pass summit from two nights ago due to strong winds.1 natural loose avalanche size 2.0 west of the summit yesterday, solar triggered.

Confidence

Intensity of incoming weather systems is uncertain on Tuesday

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.