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Avalanche Forecast

Archived

Feb 18th, 2022–Feb 19th, 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.
Below Treeline
Natural avalanches unlikely.

Regions

Jasper.

New snow and cooler temperatures should provide for some decent skiing over the weekend.Moderate rating for tree line mostly due to expected increased sensitivity of newly formed wind slabs.

Weather Forecast

  Saturday:Flurries.Accumulation: 7 cm.Alpine temperature: High -6 °C.Ridge wind west: 15 km/h gusting to 50 km/h.Freezing level at valley bottom.

Sunday:Mainly cloudy with scattered flurries.Accumulation: 4 cm.Alpine temperature: Low -23 °C, High -10 °C.Light ridge wind.Freezing level at valley bottom.

Snowpack Summary

New wind slabs in the alpine and exposed tree line from past weeks winds and incremental precipitation. Weak temperature crust up to 1900m and solar crust on solar aspects up to 2800m. December facets down 20-70cm, showing signs of rounding within bulleting region. Basal facets & depth hoar present throughout area up to 30 cm off the ground.

Avalanche Summary

Icefields patrol noticed few small wet loose slides at lower elevations, running within the new snow on Friday.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.