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Avalanche Forecast

Archived

Feb 22nd, 2026–Feb 23rd, 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.

In a sea of wind affected surfaces, lingering wind slabs remain a concern and may be tricky to recognize.

Avoid large open slopes capable of producing large avalanches.

Confidence

Moderate

  • The snowpack structure is well understood.
  • We are uncertain about how quickly the snowpack will recover and gain strength.

Avalanche Summary

No recent avalanche activity has been reported.

With limited loose snow remaining for transport, natural avalanches are unlikely. Human-triggered avalanches remain possible.

Reports in this region are limited, please post any photos or observations to the MIN if you head out!

Snowpack Summary

Outflow winds have sculpted the snowpack. Wind scoured, or hard snow surfaces exist in exposed terrain, while wind slabs have formed in lee or cross loaded features.

The January 26 crust is buried 50–100 cm deep below 1350 m. Surface hoar may linger above this layer on sheltered north to east aspects. Human triggering is considered unlikely.

Facets or depth hoar exists at the base of the snowpack and may be a concern in areas with a shallow snowpack.

Weather Summary

Sunday Night
Clear skies. 40 km/h northeast ridgetop wind. Treeline temperature -20 °C.

Monday
Mostly sunny. 30 km/h northwest ridgetop wind. Treeline temperature -14 °C.

Tuesday
Mostly cloudy. 2 to 5 cm of snow. 50 km/h southwest ridgetop wind. Treeline temperature -9 °C.

Wednesday
Mostly cloudy. 5 cm of snow. 40 km/h southwest ridgetop wind. Treeline temperature -8 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Recent strong wind means wind slabs may be found farther downslope than expected.
  • Outflow winds may form wind slabs at all elevations.

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.