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Avalanche Forecast

Archived

Feb 3rd, 2013–Feb 4th, 2013

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

Regions

South Coast.

Confidence

Good

Weather Forecast

Monday: Expect cloudy skies with a chance of flurries. Winds should be light and southerly and alpine temperatures should reach -5.Tuesday: Flurries could build to give moderate accumulations. Gusty southerly winds continue and alpine temperatures should reach -5.Wednesday: Cloudy, with light southerly winds and temperatures reaching -5.

Avalanche Summary

Isolated loose wet sluffs have been reported. The Coquihalla area has seen some glide slabs release on slopes with granite slabs as the ground cover.

Snowpack Summary

Wind slabs can be found behind ridges, ribs and on lee slopes (NW-NE). Sun crusts have formed on South and West facing slopes. The upper snowpack is showing continued settlement and gaining strength. Down 20-50 cm sits a persistent interface comprising of crusts, facets and surface hoar crystals. Recently, this layer has been reactive only  in sheltered areas at treeline and below where the surface hoar lingers. The mid pack is generally well settled. The average snowpack depth at treeline is 180 cm.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.