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Avalanche Forecast

Archived

Jan 10th, 2023–Jan 11th, 2023

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Akamina, Crowsnest North, Crowsnest South.

Continue to assess the snowpack for signs of instability and be willing to adjust plans if warranted.

Confidence

High

Avalanche Summary

No significant avalanche activity has been reported in the last couple of days.

Please continue to share any observations or photos on the Mountain Information Network.

Snowpack Summary

Up to 10 cm of snow in areas since the weekend has buried various firm layers of previously wind-affected snow or a thin melt-freeze crust. The mid snowpack is generally consolidated and sits above a weak, facetted lower snowpack.

Weather Summary

Tuesday night

Mostly clear, and no precipitation. Light southwest ridgetop winds. Treeline temperatures -5 to -10 C.

Wednesday

Mostly sunny, and no precipitation. Light to moderate southwest ridgetop winds. Treeline temperatures -5 to -10 C.

Thursday

Cloudy with flurries, and trace snow. Moderate to strong southwest ridgetop winds. Treeline temperatures 0 to -5 C. Freezing levels 1500 m.

Friday

Cloudy with flurries, and trace snow. Moderate to strong southwest ridgetop winds. Treeline temperatures around 0 C. Freezing levels 2000 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Wind slabs are most reactive during their formation.

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.