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Avalanche Forecast

Archived

Apr 15th, 2013–Apr 16th, 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.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Kananaskis.

Watch for continued reverse wind loading with persistent NE winds.NOTE: Bulletins will now be issued sporadically until the end of April.

Confidence

Fair - Due to limited field observations

Weather Forecast

Light flurries will continue Monday night, with scattered light flurries on Tuesday. Winds are expected to be moderate to strong from the East and temperatures will remain cool.

Avalanche Summary

Nothing new was observed or reported, but observations were very limited today.

Snowpack Summary

Recent storm snow continues to settle. Soft slabs are present in lee and cross-loaded features at alpine and treeline, and isolated thin slabs are also found on S aspects. Previously formed crusts persist.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

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.