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Avalanche Forecast

Archived

Apr 19th, 2023–Apr 20th, 2023

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

Regions

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

The basal facets in this area will remain a concern through the end of the season. This should be factored into terrain decisions.

Confidence

Moderate

Avalanche Summary

Several natural and cornice triggered wind and storm slabs have been reported over the past several days. A large deep release was reported out of the north side of Surprise Pass on Tuesday. Ski-hills only reported small loose dry avalanches out of steep terrain today.

Snowpack Summary

15-40 cm of snow in past week (most around Lake Louise) overlies previous storm snow at upper elevations and rain-crusts below 1800 m. Recent strong winds have created wind-slabs in the alpine. Multiple buried crusts are present in the mid-pack on solar aspects. The basal snowpack remains weak with facets and depth hoar in most areas.

Weather Summary

Thursday: Isolated showers or alpine flurries in the morning and light convective activity in the afternoon along the divide. Up to 5 cm of snow forecasted. Freezing levels between 14-1700 m. Light winds.

Friday: Flurries with minor accumulations. Winds swing to SW and increase to moderate throughout the day. Freezing levels rise to 2000 m.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Avalanche hazard may have improved, but be mindful that deep instabilities are still present.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.