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Avalanche Forecast

Archived

Dec 19th, 2025–Dec 20th, 2025

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
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 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.

The snowpack has more than doubled itself since the start of December. A Natural avalanche cycle has occurred in all avalanche terrain and is now primed for human triggering. Large full path avalanches are possible and will easily reach into below treeline elevations. Stick to low angle supported terrain with no over head until conditions improve.

Confidence

Moderate

  • Uncertainty is due to the limited number of field observations.
  • Uncertainty is due to the complexity of the snowpack’s structure.

Avalanche Summary

A field team was out along the spray today and walked in to Commonwealth valley. No new avalanches were observed. Significant evidence of previous cycle in the last 72 hours is evident in most avalanche terrain.

Snowpack Summary

This last storm has given us between 50-70cm of snow in the last 4 days. Extensive wind slabs can be found in the Alpine and lee features at treeline. These wind slabs are likely to be reactive to skier traffic. A previous wind slab from Monday can be found down about 50-80cm and was sitting on a softer layer of decomposed crystals that should be investigated for its reactivity. The November crust is now down 100+cm. Any avalanche triggered in the upper snowpack has a strong likelihood to step down to deeper instabilities. Now is a time to avoid exposure to avalanche terrain and give time for the snowpack to settle and stabilize.

Weather Summary

Some forecasts are calling for varying amounts of snow on Saturday. 2-12cm possible.

The winds will continue in the strong range (60km/h) out of the West at ridgetop. However lower down in elevation winds will be much lighter

Overnight low temp of -16 warming through the day to -11

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.

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.

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.