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Avalanche Forecast

Archived

Apr 19th, 2023–Apr 20th, 2023

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

Little Yoho.

Watch for fresh wind slabs as you transition into alpine terrain.

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. The basal depth hoar is only a concern in shallow snowpack areas. Lower elevations have a temperature crust on all aspects.

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.

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.