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Avalanche Forecast

Archived

Feb 28th, 2013–Mar 1st, 2013

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

Regions

South Coast.

Confidence

Fair - Timing, track, or intensity of incoming weather is uncertain for the entire period

Weather Forecast

Thursday night: Moderate precipitation. Strong to extreme S winds. Freezing level around 1500-1800 m.Friday: Steady, moderate to heavy precipitation. Strong to extreme SW winds. Freezing level around 1800 m.Saturday: Light to moderate precipitation. Winds easing to moderate southerly. Freezing level around1800 m, lowering to  around 1000 m.Sunday: Lingering snow showers could bring up to 15 cm snow. It may clear up. Light winds. Freezing level around 800 m.

Avalanche Summary

Almost every day this week, skiers have triggered slabs to size 2, failing on buried surface hoar/crusts which exist at all elevations and on all aspects. Some were triggered remotely, and they exhibited wide propagation. Details of some of these incidents can be found here. A natural cycle to size 2.5 occurred on Sunday night and Monday in response to new snow and wind-loading. A natural avalanche cycle is expected over the next few days in response to intense storm loading.

Snowpack Summary

Two very touchy weaknesses of surface hoar and/or a crust within the upper metre or so of the snowpack have already been responsible for a number of avalanche incidents. Add an intense storm, with heavy precipitation rates, warming and very strong winds, and we have a good recipe for widespread avalanche activity. The lower snowpack is well settled.

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.