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Avalanche Forecast

Archived

Jan 16th, 2016–Jan 17th, 2016

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 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.

Regions

Kootenay Boundary.

Extra caution required below treeline where a buried weak layer is easily triggered. Check out the new forecaster blog at avalanche.ca/blogs or click here.

Confidence

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

Weather Forecast

The next storm has arrived and should produce 5-10 cm of snow by Sunday morning. There is a break in the action on Sunday and Monday with flurries likely not amounting to more than a few cm each day. Current model runs show the interior back into a storm cycle on Tuesday with another 5-10 cm throughout the day. Freezing levels should hover around 1300m and ridgetop winds are expected to remain light to moderate out of the southwest for the forecast period. For additional weather information see avalanche.ca/weather

Avalanche Summary

Numerous natural and human triggered avalanches size 1-2.5 were reported throughout the region on Friday. These avalanches occurred at all elevations and aspects. Of note, a size 2.5 avalanche was remotely triggered from 30 m away near Rossland. This trend is expected to continue throughout the weekend as the snow load increases.

Snowpack Summary

A 40-60 cm storm slab overlays a variety of surfaces including large surface hoar, sun crusts, and facets. In recent days, the snow above this layer has settled into a cohesive slab and is ripe for human triggers. Expect this slab to be thicker on lee features in the alpine. The mid and lower snowpack are generally well settled and strong.

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.