Avalanche Forecast

Archived

Dec 27th, 2022–Dec 28th, 2022

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches possible, human triggered probable.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Natural avalanches unlikely, human triggered possible.

Regions

Kananaskis, Bow Valley, Highwood Pass, North 40, Spray - KLakes.

Recent wind and warm temps have formed wind slabs at Treeline and above. These slabs sit on a particularly weak base this winter, which will be extremely slow to improve. Backcountry users need to adopt a conservative mindset and make cautious terrain decisions for the foreseeable future.

Confidence

Moderate

Avalanche Summary

No new avalanches observed or reported today.

Snowpack Summary

Up to 5cm of fresh snow overlies a new rain crust formed yesterday up to at least 2200m. The upper snowpack has gained some density with the warm temps. Wind slabs are present in Alpine and exposed Treeline terrain, particularly just below ridgelines and in gully features. Below this new snow and wind slabs the snowpack is very weak. Forecasters are tracking the Dec 16th surface hoar/facet layer down 10 to 20cm and the mid-November facet/surface hoar/depth hoar layer down 50 to 80cm. If avalanches are initiated on these layers they will likely step to ground through the very weak basal facets/depth hoar. It's not a pretty picture!

Weather Summary

Light flurries overnight with more of the same through Wednesday. Accumulations will likely be around 5cm. Mild temps and moderate SW winds are forecasted, with a cooling trend later in the week.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
Be aware of the potential for surprisingly large avalanches due to deeply buried weak layers.
Be especially cautious as you transition into wind affected terrain.

Problems

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.

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.