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Avalanche Forecast

Archived

Apr 6th, 2026–Apr 7th, 2026

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

Regions

Banff Yoho Kootenay, Little Yoho, Banff, East Side 93N, Kootenay, Lake Louise, LLSA, Sunshine, West Side 93N, Field.

Cooling trend with light snow and strong SW wind. If snowfall exceeds forecast, wind may build small windslabs in the alpine.

Confidence

Avalanche Summary

Sunshine patrol reported a widespread, solar-driven loose wet cycle to size 1.5 in the surrounding backcountry on Monday. This occurred on all aspects and elevations, except high polar aspects.

A recreational party in Little Yoho also reported a solar-driven loose wet cycle to size 1.5 on Monday.

No cornice failures were noted; however, cornices are large and generally suspicious across the forecast region. See photo.

Snowpack Summary

Sun crusts on solar aspects extend to ridgeline. Shady aspects hold dry, settled snow above 2300 m. Temperature crusts are forming below 2300 m, with isothermal snow at lower elevations. The March 20 rain crust is 10–50 cm deep and extends to 2100–2300 m or higher. The January 24 persistent weak layer (facets over crust) is down 70–160+ cm and is becoming non-reactive. Below this, the snowpack is generally strong with no significant weaknesses.

Weather Summary

A cold front edges into the region early Tuesday morning, bringing a cooling trend. Valley temperatures drop to slightly below zero, with ridgetop temperatures near -13°C. Light snowfall is expected, with modelled totals up to 6 cm. Winds will increase into the strong range from the southwest as the front leans into the region.

Terrain and Travel Advice

  • Cornice failures could trigger large and destructive avalanches.

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.