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Avalanche Forecast

Archived

Jan 26th, 2022–Jan 27th, 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 unlikely, human triggered possible.
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.

Patience Grasshopper, nothing much has changed. The danger ratings remain Moderate due to deeply buried facets in the snowpack - especially BTL in Kootenay. Occasional huge avalanches. This is just how it is, so settle in and stay off the big slopes.

Weather Forecast

A ridge of high pressure continues to dominate the weather pattern in our region with clear skies and light-moderate NW winds forecast for Thursday. Temperatures should remain below freezing in all areas except sheltered, south and west facing slopes where there could be local warming.

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 weak (Dec 2) crust/facet interface generally 60-100cm deep. This layer continues to produce sudden test results in Kootenay Park and requires a cautious approach.

Avalanche Summary

Skiers triggered a cornice that triggered a size 3 avalanche on the east face of Mt. Carnarvon (above Hamilton Lakes in Yoho Park) on Tuesday. This stepped down to a deeper persistent layer, which illustrates that big triggers or "hitting the sweet spot" can still produce large avalanches. Nothing new reported on Wednesday.

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.