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Avalanche Forecast

Archived

Feb 8th, 2021–Feb 9th, 2021

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.

Choose your objective with the cold weather in mind. Good skiing can be found at all elevations. 

Confidence

High -

Weather Forecast

More COLD...Tuesday morning will start out around -29c and warm up to -20c by early afternoon. Expect winds out of the west at 30-40km/hr with a mix of sun and cloud. Very similar for Wednesday except for the fact that temperatures will drop down to -36c that night. Having an equipment or body breakdown in this cold can suddenly feel pretty real, pretty fast.  

Avalanche Summary

No new avalanches were observed.

Snowpack Summary

We are looking at about 60cm of settled snow from these recent storms and just over 2m total snow at tree line. The interface with the storm snow is progressively getting stronger but take the time to dig and evaluate this interface before committing to larger features. Some wind effect in the alpine and our usual concerns for lee features and cross loaded gullies.

Terrain and Travel

  • Be careful as you transition into wind affected terrain.
  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.
  • Avoid areas where the snow feels stiff and/or slabby.

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.