Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Mar 12th, 2020–Mar 13th, 2020

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.

Pay attention to wind slabs and reverse loading as you approach tree line. Good skiing can be found in sheltered areas.

Confidence

Moderate -

Weather Forecast

Cold and East winds are coming. Friday is forecast to have a high of -17c along with 5cm of snow. With the easterly winds, be on the lookout for some reverse loading. The weather models are not all in agreement with snowfall amounts for Friday and the weekend, so let's hope for more.

Avalanche Summary

No new avalanches were observed.

Snowpack Summary

Widespread buried wind slabs in the alpine and parts of treeline are found under the 10cm of snow that fell Tuesday. There are several generations of wind slabs and it is taking some time for them to consolidate into one layer. Expect some areas of surface sun crust on steep solar aspects, particularly at lower elevations. Cornices are large right now and should be given respect.

Terrain and Travel

  • Be aware of highly variable recent wind loading patterns.
  • Avoid lee and cross-loaded terrain.
  • Extra caution is needed around cornices under the current conditions.
  • Be aware of the potential for large avalanches due to the presence of a deep persistent slab.

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.