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Avalanche Forecast

Archived

Feb 24th, 2022–Feb 27th, 2022

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, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

Waterton Lakes.

Expect to find windslab in new places as winds continue to switch between NW and SW.

By the end of the forecast period a return to X SW winds and warm temps.

Weather Forecast

Friday: Clear skies and an alpine high -10. Winds L from the NW

Saturday: Temps rising to -5 with clear skies in the morning and cloud in the afternoon. Winds increasing through the day S-X SW by evening.

Sunday: Cloudy skies with temps rising to zero in the alpine. S-X SW winds at ridgetop. FL near 1700m

Snowpack Summary

Variable winds M-S forming new windslabs 10-30cm deep. This overlies pressed surfaces and old hard windslab 10-30 cm deep, or Feb crust. Feb 15 crust is 1 cm thick and exists to tree line all aspects and higher on solar aspects. Well settled midpack. Facets above Dec 4 crust, beginning to break down, buried 150-200 cm.

Avalanche Summary

A natural cycle to size 2 was observed along the Akamina Parkway yesterday. The cycle included both windslabs and dry loose avalanches. Thanks for the great observations on the Mountain Information Network, we love seeing your adventures.

Confidence

Wind speed and direction is uncertain

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.