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Avalanche Forecast

Archived

Apr 24th, 2026–Apr 25th, 2026

Alpine
Spring Conditions
Treeline
Spring Conditions
Below Treeline
Spring Conditions
Alpine
Spring Conditions
Treeline
Spring Conditions
Below Treeline
Spring Conditions
Alpine
Spring Conditions
Treeline
Spring Conditions
Below Treeline
Spring Conditions

Regions

Jasper, Brazeau, Churchill, Cirrus-Wilson, Fryatt, Icefields, Maligne, Marmot, Miette Lake, Pyramid.

An all freeze and no melt situation continues. Watch for pockets of wind slab in the alpine; they may be reactive to people, solar radiation or additional wind loading.

Confidence

Avalanche Summary

Climbers on the Icefields Parkway today reported intense wind transport in the alpine and observed a large avalanche in the Stutfield basin, a wind slab on Mt Wilson, and a serac collapse from below the Normal (Ramp) route on Mt Athabasca which ran for approximately 800m.

Another pair of climbers triggered a small wind slab while approaching the AA buttress of Mt Athabasca Friday morning.

Snowpack Summary

Since Tuesday evening, 17mm of precipitation has fallen either as snow or rain depending on elevation and timing of the cooling weather. Expect to find up to 20cm of new snow in high alpine locations.

Melt-freeze crusts exist on all aspects except North alpine, with treeline and below in transition toward isothermal. The high alpine is still holding on to a winter snowpack on NW to NE aspects with the Jan 24th PWL down 80 to 120cm.

Weather Summary

The low-pressure system sitting over the prairies may result in some precipitation on the Eastern edge of the forecast region, but most areas will experience a cloudy day with sunny breaks, North winds to 35km/h, no precipitation, and an alpine high of -5°C.

Wind speeds will taper Sunday and Monday, with freezing levels creeping up to 2000m on Monday.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.

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.