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Avalanche Forecast

Archived

Feb 11th, 2013–Feb 12th, 2013

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

Regions

Little Yoho.

Weather Forecast

A  frontal system will pass through the area on Tuesday bringing light snowfall and strong westerly winds. After the passage of the cold front  cooler temperatures and gusty northwest wind are forecasted for Wednesday. The winds and new snow will cause the avalanche hazard to increase over the short term.

Snowpack Summary

Forecasted light snowfall and strong westerly and north-westerly winds on Tuesday will create touchy windslabs in lee alpine terrain. Jan 06 surface hoar facet layer down 30-50 still producing hard planar shears. Where shallow the mid-pack is weak and facetted. In deeper snow country west of the divide the mid-pack remains strong.

Avalanche Summary

A large cornice triggered a Class 2 slab out of steep east facing terrain on Wapta Peak in past 48 hours. Otherwise no recent avalanche activity observed or reported.

Confidence

Forecast snowfall amounts are uncertain on Tuesday

Problems

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.