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Avalanche Forecast

Archived

Mar 14th, 2020–Mar 15th, 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.

Watch for multiple layers of wind slabs in wind prone areas. Solar input could be intense by Sunday afternoon. Keep an eye on localized conditions.

Confidence

Moderate -

Weather Forecast

Sunday should be sunny and warm with temps near -3 by the afternoon. Winds will shift to the SW and be light. No precipitation is expected for the next couple of days.

Avalanche Summary

Nothing new observed today, but visibility was limited.

Snowpack Summary

A couple of cm's of fresh snow in the past 24 hours. The wind slabs (numerous generations) still dominate the landscape in the Alpine and open areas at Treeline. While becoming less sensitive to human triggering, be cautious in steep, convex and unsupported terrain. The mid-pack remains quite strong, and by contrast, the basal facets are still weak. The deep persistent slabs are more of a concern in shallow snowpack areas and rocky outcroppings.

Watch for moist snow on solar aspects by Sunday afternoon. The heat could also make the triggering of some features more sensitive.

Terrain and Travel

  • Expect slab conditions to change drastically as you move into wind exposed terrain.
  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.
  • Avoid shallow snowpack areas, rock outcroppings and steep convex terrain where triggering is most likely.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.
  • Minimize exposure to sun-exposed slopes when the solar radiation is strong.

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.