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Avalanche Forecast

Archived

Dec 31st, 2022–Jan 1st, 2023

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

Akamina, Crowsnest North, Crowsnest South.

Assess for wind slabs in steep terrain prior to committing.

Confidence

High

Avalanche Summary

No avalanches were reported on Friday. A few wind slab avalanches were reported on preceding days. They include some large (size 2) natural wind slab avalanches in steep rocky terrain and some small (size 1) explosive and skier triggered wind slabs up to 50 cm thick.

Snowpack Summary

Around 20 cm of snow overlies a hard melt-freeze crust up to around 2000 m. Strong southwest wind redistributed the surface snow, forming wind slabs in lee terrain features. Moist snow or a surface crust may be found up to around 1600 m.

The middle of the snowpack is generally consolidated and sits above weak, faceted snow near the ground.

Weather Summary

Saturday Night

Cloudy with no precipitation, 20 km/h west wind, treeline temperature -5 °C.

Sunday

Mix of sun and cloud with no precipitation, 10 km/h west wind, treeline temperature -5 °C.

Monday

Mostly sunny with no precipitation, 10 km/h southwest wind, treeline temperature -5 °C.

Tuesday

Sunny with no precipitation, 10 km/h southwest wind, treeline temperature -5 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Use caution when approaching steep and rocky terrian.
  • Use ridges or ribs to avoid areas of wind loaded snow.
  • Back off if you encounter whumpfing, hollow sounds, or shooting cracks.

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.