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Avalanche Forecast

Archived

Jan 10th, 2025–Jan 11th, 2025

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.
Below Treeline
Natural avalanches unlikely.

Regions

East Kakwa, Tumbler.

Watch for signs of instability like shooting cracks and recent avalanches, especially below ridgelines and in cross-loaded features.Observations are limited, verify conditions.

Confidence

Low

Avalanche Summary

No avalanches have been reported in this area in the month of January.

Observations are almost non-existent in this area. If you are getting out in the backcountry, consider making a post on the MIN (Mountain Information Network).

Snowpack Summary

Strong wind will move any loose snow, building fresh wind slabs in the alpine and treeline. A shift from southwest to northwest wind means that wind loading will be happening on different slopes versus Wednesday and Thursday.

The snowpack in this region is expected to be much shallower and more faceted compared to areas further west.

Observations are almost non-existent in this area. If you are getting out in the backcountry, consider making a post on the MIN (Mountain Information Network).

Weather Summary

Friday Night

Cloudy with 0-2 cm of snow. 40 to 60 km/h west ridgetop winds. Treeline temperature -6 °C.

Saturday

Cloudy with 0-2 cm of snow. 30 to 40 km/h northwest ridgetop wind. Treeline temperature -6 °C.

Sunday

Sunny. 20 to 40 km/h northwest ridgetop winds. Treeline temperature -6 °C.

Monday

Mostly Sunny. 50 to 70 km/h west ridgetop wind. Possible temperature inversion above 1500 m. Treeline temperature -2 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Wind slabs are most reactive during their formation.
  • Carefully evaluate steep lines for wind slabs.
  • Use caution above cliffs and terrain traps where even small avalanches may have severe consequences.

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.