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Avalanche Forecast

Archived

Mar 23rd, 2021–Mar 24th, 2021

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

Regions

Jasper.

Good skiing can be found at elevations over 1700m. Evaluate snow and terrain carefully for changing conditions.

Expect open water BTL and plan your travel accordingly. 

Weather Forecast

The next few days will see varied conditions though the region. Winds will increase to 40-60 km/h, SW at ridge tops. Light precip, in many forms can be expected. In addition, freezing levels forecast to remain near valley bottom overnight, rising to 1500-1800m.

Wednesday: Cloudy with scattered flurries, up to 5cm. Alpine temperature: High -4 °C.

Snowpack Summary

Convective flurries and favorable SW winds have redistributed low density, new snow over hard windslab and varied crusts at TL/ALP elevations. This combination often creates a very poor bond at the interface and users should be wary of isolated slab development in open and/or steep features. Difficult travel BTL, w/ covered hazards and open water.

Avalanche Summary

No new avalanche activity observed or reported today.

Confidence

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.