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Avalanche Forecast

Archived

Mar 24th, 2021–Mar 25th, 2021

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

Banff Yoho Kootenay.

Some variability in the forecast region - pay attention to local wind effect and recent storm snow amounts to gauge the hazard.

Weather Forecast

Trace amounts of snow expected for Thursday as a weak system crosses the rockies. Ridge winds are expected to be light  Freezing levels will rise to 2000 m in afternoon.  See https://avalanche.ca/weather/forecast for more details.

Snowpack Summary

15-40 cm of snow has fallen at treeline since March 19th with variable SW-NW winds. This storm snow sits over a sun crust (up to ridge tops) on solar aspects, and over a mix of surfaces on North aspects including facets and spotty surface hoar, and over a temperature crust at lower elevations. Thin areas becoming isothermal below treeline.

Avalanche Summary

Few small wind slabs in the high alpine were ski cut in the Sunshine area today and some loose dry to size 1.5 in steep NW alpine features in Little Yoho during a snow squall event.

Confidence

Due to the number and quality of field observations

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.