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Avalanche Forecast

Archived

Mar 13th, 2013–Mar 14th, 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 and human triggered avalanches likely.
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

Kananaskis.

Precipitation and wind forecasts have been highly variable and we have received less snow and wind than predicted.  The new snow forecast for Thursday night will push us into a higher danger rating if it does show up - watch for rain effects to 2100m

Confidence

Fair - Timing, track, or intensity of incoming weather is uncertain on Thursday

Weather Forecast

Winds strong west with freezing level forecast in the 2100m range (we have seen freezing levels rising to 2250m in the Burstall area Wednesday PM).  The area has received less new snow than the precip forecast predicted but there is another spike predicted for Thursday night with up to 15cm+ possible.

Avalanche Summary

Numerous loose, moist slides from steep lee terrain.  One Size 2 SSL NE aspect Mt Smith-Dorrien, no other details.

Snowpack Summary

Up to 10cm of new snow at treeline with temperatures rising above zero degrees so rapid settlement and slab formation.  Winds were generally light with occasional periods of strong southerly winds resulting in some redistribution of storm snow along ridgetops.  

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.