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Avalanche Forecast

Archived

Feb 13th, 2021–Feb 14th, 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, 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

Jasper.

The facet-fest continues, and the snow pack continues to loose strength.

Weather Forecast

Sunday: A mix of sun and cloud. Precipitation: Nil. Alpine temperature: High -15 °C. Ridge wind southwest: 10 km/h.

Monday: A mix of sun and cloud. Precipitation: Nil. Alpine temperature: Low -17 °C, High -9 °C. Ridge wind west: 10 km/h.

Snowpack Summary

The cold weather continues to promote facetting of the upper 40cm. The mid-pack is showing signs of losing strength with the prolonged arctic influence, especially where it is shallow. Widespread wind effect in the alpine and upper tree line.

Avalanche Summary

Road patrol on Feb 13 observed numerous Natural Loose Dry Avalanches up to size 1.5, starting steep terrain, but running the distance in terrain over 30 deg. One size 2 serac triggered wind slab, up to a meter deep, was also directly observed.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.

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.