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Avalanche Forecast

Archived

Feb 26th, 2020–Feb 27th, 2020

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, 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.

Daily flurries are helping to refresh the ski quality. North facing, sheltered areas are the best bet for good turns.

Confidence

High -

Weather Forecast

Remember yesterday's weather? Well, tomorrow will be like that. Cloudy skies with flurries, daytime high of -6 and light, but gusty winds. 

Avalanche Summary

Nothing new today.

Snowpack Summary

Convective flurried continue to roll through, but accumulation is minimal given the sun peaking through the clouds. The windslabs continue to pile up on top of themselves with continued SW winds. There may be pockets of new slabs that are slow to bond, but generally they seem to be quickly settling out and staying where they are supposed to. We do have a couple of crusts to deal with on south aspects and lower elevation areas.

Terrain and Travel

  • Avoid convexities, steep unsupported terrain and rocky outcroppings.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.
  • Watch for areas of hard wind slab on alpine features.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.