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Avalanche Forecast

Archived

Dec 2nd, 2015–Dec 3rd, 2015

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

Regions

Glacier.

The calm, sunny weather has ended. The stormy weather will usher in change to the mountains.

Weather Forecast

Expect flurries with light to moderate SW winds today, freezing levels remaining in the valley bottom around Rogers Pass. Thursday will bring more snow, but models are in disagreement on amounts: 10 to 25cm could fall. Freezing levels will rise to 1600m on Thursday, with strong SW winds.

Snowpack Summary

5cm of new snow has hidden various surfaces. 20mm surface hoar and surface facetting was prevalent below tree-line. At tree-line and above, 6mm surface hoar was found with sun crusts on steep solar aspects, variable wind effect and slabs in exposed terrain. The low elevation surface hoar and facetting will be a layer to watch with future loading.

Avalanche Summary

No new avalanches observed yesterday.

Confidence

Due to the number of field observations

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.