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Avalanche Forecast

Archived

Apr 3rd, 2015–Apr 4th, 2015

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

Regions

Kootenay Boundary.

Snowpack and avalanche observations are becoming scarce. If you've been in the backcountry, please tell us what you've seen via the Mountain Information Network. For more details, click here.

Confidence

Fair - Intensity of incoming weather systems is uncertain on Saturday

Weather Forecast

On Saturday, expect light snowfall (up to 8cm). On Sunday, we should see a mix of sun and cloud. Light flurries are forecast for Monday. Ridgetop winds should be moderate from the southwest with Saturday's pulse, becoming light for the rest of the period. Daytime freezing levels should remain at about 1700m.

Avalanche Summary

No new avalanches have been reported, although I'm sure there has been some smaller wind slab activity in higher elevation lee terrain in response to recent snow and wind.

Snowpack Summary

Generally light amounts (1-10cm) of new snow overlie a supportive melt-freeze crust. At higher elevations these accumulations have been blown around by variable winds and new wind slabs may exist on a variety of aspects. The mid-March crust/facet complex is buried around 50cm below the surface. This layer is generally considered dormant as long as cooler temperatures prevail. The mid and lower snowpack are strong and well settled.

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.

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.