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Avalanche Forecast

Archived

Apr 11th, 2023–Apr 12th, 2023

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

Regions

Little Yoho.

A major avalanche cycle occurred in the forecast region Tuesday afternoon with slides up to size 3.5. Conditions will be ripe for human triggering on Wednesday.

Confidence

Moderate

Avalanche Summary

A cycle up to size 3.5 peaked Tuesday afternoon. Most major avalanche paths ran full path in the Banff area. Included are Cascade Waterfall, Urshole Gully, Professors, and Bourgeau Left. Lake Louise patrol also reported a widespread cycle in the immediate backcountry with deep slabs observed in Purple Bowl and Redoubt Bowl size 2.5.

Snowpack Summary

Up to 40cm of storm snow in the alpine (end of day Tuesday) overlies previous windslabs and suncrusts with rain saturated snow below 1800m. Storm slabs can still be expected in the alpine and tree-line areas.

Several buried crusts can be found in the top 50-60 cm on solar aspects. The November depth hoar at the base of the snowpack remains a concern only in shallow areas of the Yoho sub-region.

Weather Summary

Diminishing wind into the light range is expected on Wednesday. There is a possibility of localized convective flurries, with amounts potentially up to 10cm. Valley temps should be slightly above zero, with alpine temps holding steady around -10.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.