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Avalanche Forecast

Archived

Nov 28th, 2013–Nov 29th, 2013

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

Regions

Glacier.

Rocks, stumps, and crevasses still lurk beneath the shallow, early-season snowpack.

Weather Forecast

High overcast, light winds, and nil precipitation is forecasted for today. Freezing levels to rise to 1900m. Tomorrow and Saturday, we may see scattered flurries, with up to 5cm of accumulation, and light westerly ridge-top winds. Freezing level to drop to 1500m.

Snowpack Summary

Little change from yesterday, with continued settling of the snowpack, exposing more early season hazards. Sun crusts exist on steeper south/southwest aspects. Wind-pressed soft slab and facets overlay the November 12 surface hoar layer in tree-line and alpine areas. The surface hoar is down between 40-100cm at higher elevations.

Avalanche Summary

No new significant activity observed from previous 24 hours. Older crown-lines to size 2 were observed near the top of the Youngs Peak Headwall, likely 72+ hours old.

Confidence

Due to the number and quality of field observations

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.