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Avalanche Forecast

Archived

May 24th, 2014–May 24th, 2015

Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.
Alpine
Below Threshold.
Treeline
Below Threshold.
Below Treeline
Below Threshold.

Regions

Kananaskis.

Regular bulletins have stopped for the season. Summer is right around the corner and the snow pack is dwindling by the day. Large alpine features that still hold snow have yet to go through a large cycle. Watch those areas in the weeks to come.

Weather Forecast

Avalanche Summary

Snowpack Summary

We are on the verge of the summer season now and the snowpack has either disappeared, or become entirely isothermal. The high alpine is lagging a bit behind, but the freeze/thaw cycles that tend to stabilize the snowpack have been underway for awhile now.

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.