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Avalanche Forecast

Archived

Feb 5th, 2024–Feb 6th, 2024

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

Regions

Kootenay Pass, Ymir, Crawford, Moyie, St. Mary, Kokanee, Retallack.

A bit of new snow and wind Monday night will build fresh wind slabs in higher elevation terrain.

Confidence

Moderate

Avalanche Summary

There were a few skier controlled size 1 storm slab and dry loose avalanches reported from steep terrain on Monday.

Snowpack Summary

10 - 20 cm of new snow has accumulated over a crust at most elevations. Below 1500 m surface snow is likely moist or wet.

A layer of facets (and small surface hoar in some areas) is buried 30-60 cm deep and a layer of facets sitting on a crust is buried 80-100 cm deep. While previous warming and subsequent cooling have likely helped to strengthen these layers, we will continue to monitor them for signs of reactivity.

Weather Summary

Monday Night

Mainly cloudy with 3 to 8 cm. Wind southeast and southwest 15 to 35 km/h. Treeline temperature -4 °C. Freezing level 1000 m.

Tuesday

Mainly cloudy with 3 to 5 cm of snow. Wind southwest 20 to 40 km/h. Treeline temperature -3 °C. Freezing level 1100 m.

Wednesday

Mainly cloudy with 2 to 5 cm of snow. Wind southwest 15 to 25 km/h. Treeline temperature -1 °C. Freezing level 1500 m.

Thursday

Mainly cloudy with 1 to 2 cm of snow. Wind southwest 5 to 15 km/h. Treeline temperature -5 °C. Freezing level 500 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • 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.