Avalanche Forecast

Issued: Mar 24th, 2015 9:16AM

The alpine rating is considerable, the treeline rating is moderate, and the below treeline rating is low. Known problems include Storm Slabs and Persistent Slabs.

Avalanche Canada swerner, Avalanche Canada

A complex and unpredictable snowpack exists, especially in the northern half of this region. Natural and human triggered, large avalanches continue to occur.

Summary

Confidence

Fair - Timing of incoming weather systems is uncertain

Weather Forecast

The next Pacific frontal system will reach the coast tomorrow. The front will affect most of the Interior through the forecast period. Wednesday will see light convective flurries, moderate ridgetop winds from the SW and freezing levels near 1700 m. For Thursday, precipitation amounts expected are 10- 20 mm. Ridgetop winds will be strong from the SW and freezing levels rising to 2500 m. Warm air will remain over the region on Friday with freezing levels rising to 3000 m. Skies will show a mix of sun and cloud and ridgetop winds will be moderate strong from the SW.

Avalanche Summary

On Tuesday afternoon we received a report of a human triggered persistent slab avalanche size 2.5 on a northerly aspect at 2000 m. On Monday, numerous natural and human triggered slab avalanches were reported up to size 2.5 with the majority failing in the recent storm snow and the deeper mid-March interface. There were several remotely triggered avalanches with the farthest being triggered from 150 m away. On Wednesday, I suspect natural avalanche activity to taper off; however, remote human triggering remains a major concern up to size 2.5. Avalanches that fail on the deeper weak interfaces will be large and destructive.

Snowpack Summary

At higher elevations, 40-60 cm of dense storm snow sits over the mid-March interface which had included crusts, moist snow, wind affected surfaces, and/or old wind slabs. This interface has recently come alive and is reactive, especially in the North (Revelstoke and surrounding area). Recent snowfall amounts taper off towards the south of the region. Strong SW winds had redistributed the new snow into wind slabs on leeward features. Digging deeper, 50-80 cm is the mid-February facet/crust interface. There is some concern for this layer to wake-up in the South Columbia region and storm slab avalanches have the potential to step down to it. Snow surfaces are wet to around 1700 m and moist to around 2200 m. The snow surface is undergoing melt-freeze cycles as freezing levels drop overnight.

Problems

Storm Slabs

An icon showing Storm Slabs
Storm slabs up to 60 cm thick may overlie a weak layer and remain reactive to human-triggering. These slabs may be moist or wet at lower elevations.
Use conservative route selection, stick to moderate angled terrain with low consequence.>Avoid steep, open slopes.>

Aspects: All aspects.

Elevations: All elevations.

Likelihood

Possible - Likely

Expected Size

1 - 3

Persistent Slabs

An icon showing Persistent Slabs
A persistent weak layer is buried anywhere from 40-80 cm below the surface and has produced numerous large avalanches recently. Storm slab avalanches could easily step down to this layer and remote triggering is possible.
Be aware of the potential for wide propagations and remote triggering due to a buried weak layer.>

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible - Likely

Expected Size

3 - 5

Valid until: Mar 25th, 2015 2:00PM

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