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Avalanche Forecast

Archived

Jan 15th, 2018–Jan 16th, 2018

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

Regions

Jasper.

Weather Forecast

Pacific air will continue to override cooler air in the valleys producing a temperature inversion through to Tuesday. Winds should remain light from the SW through Monday until late in the day Tuesday when they will increase and potentially bring some light flurries or rain. 10mm of precipitation with moderate SW winds expected to arrive mid-week.

Snowpack Summary

10-15cm of recent snow has blown into thin slabs TL and above. Although the mid-pack Dec 15 layer of concern has not been reactive in test profiles (nor has it been tied to any recent avalanche activity in the Jasper area), we are still monitoring this interface closely. There is still a distinct crust (Nov 17) in the lower third of the snowpack.

Avalanche Summary

Another pulse of natural loose dry point releases was observed today in the Columbia Icefield area and in the Maligne Valley. These slides were mostly out of steep, solar facing terrain. Field teams did not observe any new slab avalanches avalanches.

Confidence

Intensity of incoming weather systems is uncertain

Problems

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.

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.