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Avalanche Forecast

Archived

Dec 20th, 2017–Dec 21st, 2017

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

Recent winds and new snow have loaded lee features in the alpine.  Good skiing can be found throughout but should be approached with caution for wind slabs.

Confidence

High -

Weather Forecast

Thursday is expected to bring cloudy skies with flurries (5cm) and alpine temperatures of -10.  The wind should be steady around 20km/hr from the west.

Avalanche Summary

No new avalanches were observed. 

Snowpack Summary

8cm of new snow overnight brings our storm snow to about 25-30cm at treeline and up to 40cm in the alpine. The winds have been transporting snow in the alpine all day, so expect wind slab development around ridges and lee features.  It is possible that this wind effected snow extends to tree line as yesterday had winds from all directions.

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.