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Avalanche Forecast

Archived

Feb 13th, 2025–Feb 14th, 2025

Alpine
Natural avalanches unlikely, human triggered possible.
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

Banff Yoho Kootenay, Banff, East Side 93N, Kootenay, Lake Louise, LLSA, Sunshine, West Side 93N, Field.

Finding areas where there is no significant wind effect and/or lingering wind slab will lead you to the safest and most enjoyable travel.

Confidence

High

Avalanche Summary

On Thursday, Sunshine Village reported numerous small size 1 windslab avalanches with explosive control. Otherwise, no new avalanches were reported.

On Tuesday we investigated the Quartz skier accidental avalanche, where the start zone was 48° and the failure plane was an old layer of weak facets down 50 cm. The avalanche was triggered from a very shallow, faceted location and the crack propagated into the thicker snowpack nearby and released the avalanche.

Snowpack Summary

Last weeks storm snow has been redistributed into now aging wind slabs, which sit on top of the Jan 30 interface. Specific areas exposed to the wind may also have strastrugi. The mid-pack is generally weak with facets, while depth hoar over a crust forms on an even weaker base. The snowpack is the weakest in eastern areas where snow depths are low. In these areas, the basal weaknesses should be carefully considered. Here is a representative snow profile taken on Wednesday

Weather Summary

Thursday night: Cloudy with clear periods. Alpine temperature: Low -15 °C. Ridge wind east: 10 km/h. Alpine temperature inversion.

Friday Mainly cloudy. Alpine temperature: High -15 °C. Ridge wind east: 10 km/h.

Saturday Cloudy with sunny periods and isolated flurries. Alpine temperature: Low -17 °C, High -15 °C. Ridge wind west: 10 km/h.

Terrain and Travel Advice

  • Be careful as you transition into wind-affected terrain.
  • Be mindful that deep instabilities are still present in the snowpack.
  • Closely monitor how the new snow is bonding to the old surface.

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.