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Avalanche Forecast

Archived

Apr 4th, 2018–Apr 5th, 2018

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

Regions

Kananaskis.

Light flurries are forecast for thursday before a largre pulse of snow arrives on the weekend.  Use caution in lee features in alpine terrain.

Confidence

High -

Weather Forecast

Mainly cloudy skies with isolated flurries is forecast for thursday with temperatures in the -10C to -12C range.  Winds are forecast to be light out of the east.

Avalanche Summary

No new avalanches were observed over the past 48hrs.

Snowpack Summary

Windslabs are being found in Alpine areas along ridgelines and cross loaded features. We are certainly avoiding steeper unsupported features such as above cliff walls and convex rolls that are near the entrances to some runs and terrain features. On solar aspects the march 15th crust is down 40-60cm and the bond on this crust has been variable. Did down and check this interface if you plan on moving onto more solar aspects. The skiing is likely not great on these aspects due to the presence of thin surface crusts.

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.

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.