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Avalanche Forecast

Archived

Jan 23rd, 2026–Jan 24th, 2026

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Below Threshold.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Below Threshold.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Below Threshold.

Regions

Yukon, Tutshi, Wheaton, White Pass East, White Pass West.

With little change happening in the weather, little has changed in the avalanche conditions.

A weak layer may still produce avalanches, be careful in shallow areas.

Confidence

High

  • We are confident due to a stable weather pattern.
  • We are confident that there are persistent slabs in the snowpack, but uncertain about how likely they are to trigger.

Avalanche Summary

January 16 to 23

  • No new avalanches reported but observations are limited. Consider posting to the MIN if you are out in the mountains!

Snowpack Summary

The upper 30 to 40 cm has been significantly altered by extreme southerly wind with scoured south facing slopes and loaded, pressed and sculpted, north facing slopes.

Below 1300 m and on south facing slopes a crust is present on or under the recent snow. This crust has a layer of surface hoar that is growing on it.

A weak layer of facets is buried 80 to 150 cm deep. In shallow snowpack areas, the bottom half of the snowpack is composed of weak depth hoar.

Weather Summary

Friday Night
Mainly clear skies. 20 km/h southwest ridgetop wind. Treeline temperature -7 °C. Above freezing layer from 1500 to 2000 m.

Saturday
Sunny. 20 km/h west ridgetop wind. Treeline temperature -5 °C.

Sunday
Mostly sunny. 1 cm of snow. 30 km/h west ridgetop wind. Treeline temperature -10 °C.

Monday
Mostly cloudy. 1 to 4 cm of snow. 60 km/h southwest ridgetop wind. Treeline temperature -9 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid areas with a thin or variable snowpack.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

Problems

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.