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Avalanche Forecast

Archived

Jan 27th, 2022–Jan 28th, 2022

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

Regions

Little Yoho.

There is still a lot of uncertainty around the deeper facets in the snowpack. It is very difficult to assess slopes with these types of layers. Your terrain choices will be the best risk management.

Weather Forecast

Alpine temperatures will be warmer than valley bottom on Friday, but will stay below freezing. Winds will increase 60-80km in the alpine from the West and no new snow. Slightly cooler temperatures, diminished winds, and no snow for Saturday.

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 is good skiing. Facets and a weak mid-pack remain the dominant concern and the Dec 2 crust is down 100-150 cm and producing hard test results in most of Yoho.

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 Thursday.

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.