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Avalanche Forecast

Archived

Feb 24th, 2013–Feb 25th, 2013

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
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

Cariboos.

Confidence

Fair

Weather Forecast

Synopsis: A weather system affecting the region on Sunday will move out and leave behind unsettled conditions for Monday. A ridge of high pressure is expected to form and give drier conditions with sunny breaks for late Monday and Tuesday. Overnight and Monday: Continued moderate to locally heavy snowfall – 10-20 cm through Monday. The freezing level is around 900 m during the day and winds are moderate from the southwest, easing to light from the west.Tuesday: A mix of sun and cloud. The freezing level is around 800 m and winds are light from the southwest.Wednesday: Light to moderate snow. The freezing level should remain near 800 m.

Avalanche Summary

Surprisingly there were few reports of slab avalanches from the region over the past couple days. Just to the southeast in the northern Monashees and Selkirks there was a fairly widespread natural avalanche cycle in response to heavy snow and strong wind on Friday.

Snowpack Summary

40-70 cm of new snow has fallen in the past few days. Strong west-southwest winds have redistributed the new snow into deep wind slabs on exposed lee slopes and cross-loaded gully features. The February 12 persistent weak layer (crust, and/or surface hoar) is now down 60-80 cm and is primed for triggering. Recent snowpack tests have shown easy to moderate "pops" results on this interface and has been particularly touchy on south aspects where a sun crust exists. Deeper persistent weak layers from early February and late January continue to show planar failures when moderate to hard forces are applied in snow pack tests. These deeper layers have not been reactive to the weight of a rider, but they may be triggered by large loads like an avalanche in motion (step-down avalanche), or a cornice fall.

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.