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Avalanche Forecast

Archived

Mar 20th, 2013–Mar 21st, 2013

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

Regions

Cariboos.

Confidence

Fair - Forecast snowfall amounts are uncertain on Thursday

Weather Forecast

Overnight and Thursday: Winds becoming Westerly moderate to strong overnight as the snow continues to fall across the region. Expect another 5-15 cms overnight and another 5 cms during the day. Alpine temperatures should drop down to near -10.0, and the freezing level should be at valley bottoms.Friday: Unsettled weather with mostly cloudy skies and strong to very strong gusty Northwest winds. Continued cool temperatures in the alpine and freezing levels rising to about 1000 metres during the day.Saturday: A ridge of High pressure is moving into the region bringing light West winds, clearing skies, and alpine temperatures in the -10.0 - -15.0 range.

Avalanche Summary

A couple of natural cornice falls were reported size 3.0 that released old storm snow slabs from the sloped below. Some skier controlled pockets of wind transported snow were reported up to size 1.5

Snowpack Summary

Strong winds and new snow have developed new storm slabs on all aspects and at all elevations. Wind transported snow has created thick pockets of wind slab in the lee of alpine winds. New cornice growth may be extensive and weak, causing natural cornice falls. Buried sun crusts on Southerly aspects continue to produce planar fractures in snow profile tests down about 80-100 cms. Large avalanches releasing on the March 10th weak layer are still a concern.

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.

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.