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Avalanche Forecast

Archived

Mar 16th, 2013–Mar 17th, 2013

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

Regions

Jasper.

20 cm of snow expected overnight.  If more snow falls than expected, the avalanche danger will rise to High in the Alpine. 

Weather Forecast

Heavy snow to begin Saturday night with 20 cm expected.  Winds will shift to northerly and will drop to light.  Temperatures will fall as the snow begins.  The storm will be short lived and be finished sometime before noon on Sunday.  By Sunday afternoon the winds will shift back to light westerly, with cool temperatures and light flurries.

Snowpack Summary

Soft slabs have formed immediate below alpine ridgelines from previous moderate to strong West winds. 80+cm of snow has fallen since Wednesday. At treeline, soft slabs are sitting on a thin suncrust that is buried 80 cm deep in wind exposed south facing terrain.  Below treeline, 20-30 cm of unconsolidated snow is present over a base of weak facets.

Avalanche Summary

Large natural slab avalanches have run on steep alpine slopes.  Several large cornice failures have been observed in the past 48 hrs.  At treeline and below, mild temperatures and solar exposure provided the trigger for small loose wet slides south of the Icefields.

Confidence

Forecast snowfall amounts are uncertain on Sunday

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.

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.