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Avalanche Forecast

Archived

Jan 29th, 2022–Jan 30th, 2022

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

Regions

Banff Yoho Kootenay.

The danger remains Moderate due to uncertainty around the deeper facets, especially in Kootenay. It is very difficult to estimate whether a slope will avalanche with these types of layers. Your terrain choices will be the best risk management.

Weather Forecast

The ridge of high pressure will break down Sunday as a westerly low move into the forecast region. This low pressure system will bring 5 to 15cm of snow with higher accumulation amount to the western part of the region. By Monday evening an Arctic cold front will cool things off dropping overnight lows down into the -30s.

Snowpack Summary

Wind effect and wind slabs in the alpine and exposed tree-line areas and suncrust on steep south facing terrain. In sheltered areas, 20-40 cm of soft snow overlies facets and a (Dec 2) crust/facet interface generally 60-100cm deep. This layer continues to produce sudden test results in Kootenay Park.

Avalanche Summary

No new avalanches observed or reported on Saturday. Over the past week we have received reports and observed a few avalanche to size 3 on the persistent weak layer. All of these avalanches were triggered by large loads (cornice).

Confidence

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.

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.