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Avalanche Forecast

Archived

Apr 1st, 2014–Apr 2nd, 2014

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

Regions

Jasper.

Weather Forecast

Cool overnight temperatures, light Southwest winds and only light scattered precipitation expected over the next 48hours. Freezing levels remain below treeline.

Snowpack Summary

45cm of storm snow continues to settle and has minimal wind affect in most places.

Avalanche Summary

Skier accidental sz 2.5 reported from the Shangri-La area today, triggered remotely from a shallow spot and stepped down to ground.  Avalanche control work in the Columbia Icefield area produced mainly storm slabs in the size 2 range and isolated larger avalanches up to size 3 that failed on ground. Widespread natural cycle in the past 24 hours. 

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.

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.