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Avalanche Forecast

Archived

Mar 7th, 2013–Mar 8th, 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

Sea To Sky.

Confidence

Fair - Timing or intensity of solar radiation is uncertain on Friday

Weather Forecast

Friday: Mix of sun and cloud / Light northwest winds / Freezing level at 1200mSaturday: Clear skies / Light northwest winds / Freezing level at 1500mSunday: Light snowfall / Moderate southwest winds / Freezing level at 1200m

Avalanche Summary

A couple of skier-triggered size 1 wind slabs were observed on Wednesday. The occurred on west/southwest facing terrain at treeline and above. The effect of the sun is somewhat uncertain on Friday/ Saturday. If it is strong, expect wet snow instabilities with the potential to trigger deeper persistent weaknesses.

Snowpack Summary

Light snowfall overlies wind slabs in exposed areas, surface hoar or facets in sheltered locations, or a sun crust on south facing terrain.Below the surface, recent accumulations of 70-120cm continue to settle and strengthen. Snowpack tests are still giving generally moderate shears at various density changes within the storm snow, but triggering these instabilities has become more difficult. A weakness of surface hoar and/or a crust exists near the base of the storm snow (now 1-2 m deep in some locations). This layer was the culprit in most of the large avalanches that occurred last weekend. This layer could still be triggered in shallow rocky areas or by large triggers like a cornice fall. I would suggest avoiding any large slope that did not release during the latest avalanche cycle, especially with forecast solar warming. Below this interface, the snowpack is strong and well settled.

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.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.