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Avalanche Forecast

Archived

Dec 16th, 2025–Dec 17th, 2025

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

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

"CONTINUED HIGH AVALANCHE HAZARD"

Avoid all avalanche terrain. A storm pushing through Tuesday night and Wednesday morning will bring heavy snow and strong winds, which will overload the snowpack.

Confidence

Moderate

  • Uncertainty is due to the timing, track, & intensity of the incoming weather system.

Avalanche Summary

A natural avalanche cycle continues with slab avalanches up to size 3 in Alpine and Treeline terrain. These slabs are anywhere between 20 and 100cm thick, including many that are stepping down to the Nov crust layer. Explosives control work on EEOR today also produced several size 2 avalanches. With the incoming storm Tuesday night and Wednesday morning, a natural avalanche cycle is expected to continue.

Snowpack Summary

Incoming new snow and strong winds will add to existing wind slabs at Treeline and above. There is already a 25-40cm thick surface wind slab, and this will grow. Unfortunately, this is sitting on a softer layer of decomposed particles that is very reactive to field tests. If this layer is triggered, there is a strong likelihood that it will step down to the November crust (now buried 90-120cm), creating large avalanches. At 2200m and below the incoming snow will land on a rain/temperature crust from the last few days. The bond at this interface will be important to watch, as the crust could form a good sliding layer.

Weather Summary

Wednesday is expected to be overcast and snowy. Total accumulations should be in the neighbourhood of 25cm. With the passing of a cold front, the winds will be strong from the SW switching to the NW, and temperatures will drop from -4C in the morning to -12C in the evening.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid avalanche terrain during periods of heavy loading from new snow, wind, or rain.
  • Avoid areas with overhead hazard.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.