Avalanche forecast

Sugarbowl

Jan 29 – 30, 2026Avalanche Canada
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Archived · expired 8 months ago

Avalanche danger

Sat
Sun
Alpine
2 · Moderate
Treeline
2 · Moderate
Below
1 · Low

Highlights

Recent snow and strong winds are forming small wind slabs over surface hoar and crust.

Watch for signs of instability, like shooting cracks, in steep terrain.

Avalanche problems

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible - Likely
    Size
    1–1.5

    Recent storm snow accumulated in the Pine Pass and McGregors areas, coupled with moderate to strong winds likely formed small slabs at upper elevations. Slabs may be building over a surface hoar layer, making them more reactive.

Confidence

Snowpack Summary

Around 10 - 15 cm of recent snow is being redistributed by strong southerly winds, building small wind slabs over a layer of surface hoar.

This surface hoar layer sits on a crust found on all slopes except shaded north-facing ones, where there is a mix of soft snow from surface faceting and wind-affected snow in open terrain features.

Strong southerly winds have stripped the snowpack down to hard old surfaces and rock in exposed alpine terrain. Cornices are large and overhanging.

The lower snowpack is well settled, with the mid-December facet/crust layer buried down approximately 100 to 150 cm.

Weather Summary

Wednesday Night
Partly cloudy. 2 to 3 cm of snow. 50 km/h southwest ridgetop wind. Treeline temperature -3 °C. Freezing level 1100 m.

Thursday
Mostly cloudy. 3 cm of snow. 50 km/h southwest ridgetop wind. Treeline temperature -2 °C. Freezing level 1200 m.

Friday
Mostly cloudy. 10 - 15 cm of snow. 60 km/h southwest ridgetop wind. Treeline temperature 0 °C. Freezing level 1500 m.

Saturday
Mix of sun and clouds. 1 to 3 cm of snow. 50 km/h west ridgetop wind. Treeline temperature -2 °C. Freezing level 1200 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.
  • Carefully evaluate steep lines for wind slabs.
  • Make observations and continually assess conditions as you travel.
  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.

Regions covered