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Avalanche Forecast

Archived

Feb 17th, 2014–Feb 18th, 2014

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

Regions

South Columbia.

Confidence

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

Weather Forecast

Synopsis: Another pacific frontal system passes over the region late Tuesday accompanied by robust SW winds. Freezing levels should drop behind the system as isolated flurries linger in its wake.Tuesday: Freezing Level: 800m; Precip: 3/7mm - 4/10 cm; Wind: Light, SW | Mod/Strong SW at ridgetopTuesday Night: Precip: 5/8mm - 7/12 cm; Wind: Mod SW | Strong/Extreme SW at ridgetop Wednesday: Freezing Level: 700m; Precip: Trace; Wind: Light, West | Strong West at ridgetopThursday: Freezing Level: 600m; Precip: Trace; Wind: Light, SW

Avalanche Summary

An ongoing natural avalanche cycle has tapered ever so slightly but still features natural avalanches to size 3 with control work producing similar results. Skiers and sledders continue to easily trigger avalanches in seemingly benign terrain to size 1.5. This activity is occurring on all aspects and elevation bands.On Saturday, an avalanche fatality occurred near Revelstoke.

Snowpack Summary

The never ending storm has produced 100 - 150 cm of total snowfall across the region which is settling into a cohesive slab that averages a meter in depth. This slab rests on a nasty persistent weak layer (Late Jan/Early Feb.) surface hoar/facet/crust combo that was formed during the month of cold clear weather. Field observations continue to report easily triggered sudden planar failures on this interface in snowpack tests. Natural avalanches have been widespread and destructive. The keyword in Persistent Weak Layer is Persistent, I expect touchy conditions to remain in place longer than we're normally accustomed to due to the pervasive nature of this weakness. Ongoing strong winds out of the SW and W have loaded lee aspects and affected the snow at all elevations, but the affect is most prevalent at and above treeline. More strong winds in the forecast are expected only to add to this problem.For the most part, the mid and lower snowpack are strong and well consolidated.

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.