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Avalanche Forecast

Archived

Nov 26th, 2017–Nov 27th, 2017

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Jasper.

Icefields Parkway is closed from Saskatchewan Crossing to Athabasca Falls due to planned avalanche control. Check Alberta 511 for updated opening time.

Weather Forecast

15cm of storm snow with a further 15 to 20 cm forecasted overnight for Sunday. Snow to continue through until Tuesday afternoon. Cool alpine Temperatures up to -5. Strong to Moderate SW winds with gusty extreme winds to accompany this the remainder of the storm cycle.

Snowpack Summary

30cm of recent storm snow over a 10cm hard crust with more coming. A persistent slab between 40cm - 150cm thick sits on the Halloween Crust, low in the snowpack. This crust can be found up to 2,700m depending on its location. Wind and storm slabs likely exist in the upper alpine.

Avalanche Summary

Field team on Sunday monitoring growing storm slab over the Black Friday crust down 35cms. No new avalanches observed on the crust but visibility poor above TL. On Nov. 22nd a field team remote triggered 3 simultaneous size 2 persistent slabs 60-150m away on either side of the wind scoop at parkers ridge.

Confidence

Problems

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.

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.