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Avalanche Forecast

Archived

Jan 20th, 2025–Jan 21st, 2025

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

Regions

Little Yoho.

No change from yesterday as we are under the influence of a cold ridge of high pressure which is keeping the snowpack static. In areas of the eastern Rockies, locally strong winds were actively reloading and creating size 1 windslabs in steep north-facing terrain. This condition is not widespread but could catch someone by surprise.

Confidence

Moderate

Avalanche Summary

No avalanches were observed or reported in Little Yoho today.

Snowpack Summary

Wind slabs remain on lee features in the alpine. The upper pack may have a thin crust under the new snow on solar aspects and a surface hoar/facet interface under last week's snow, but no avalanches observed on this layer yet. The mid-pack is generally strong; however, a facet layer can be found near the ground in shallow snowpack areas. At treeline, average snowpack depth ranges from 120 to 150 cm.

Weather Summary

A ridge of high pressure is established over the region with cold air from the north keeping temperatures low. On Tuesday, a weak system will cross through, giving some overcast skies, light flurries and wind, but nothing significant before the ridge establishes itself again and clear skies return for Wednesday. Temperatures on Tuesday should reach a high of -8 in the valley bottom, so still cool.

Terrain and Travel Advice

  • Wind slabs are most reactive during their formation.
  • 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.