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Avalanche Forecast

Archived

Dec 6th, 2013–Dec 9th, 2013

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

Regions

Waterton Lakes.

Weather Forecast

Very cold temperatures continue for the forecast period. Although forecast winds are light, windchill is a big factor. Winds are forecast to pick up from the north on sunday.

Snowpack Summary

Little Prairie 63cm. Summit Lake = 100-120 cm . Cold temps have prevented slab development in the storm snow. Windslabs built during storm are present on reverse locations (northeast aspects) and could possibly be skier triggered. The facet/melt freeze interface from Dec 1 has also not settled out yet.

Avalanche Summary

Sluffng out of very steep terrain.

Confidence

Wind effect is extremely variable

Problems

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.

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.