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Avalanche Forecast

Archived

Mar 22nd, 2014–Mar 23rd, 2014

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

Regions

Little Yoho.

Great ski quality in most areas, but these are not typical March conditions. The persistent nature of the Feb.10th layer does not instill confidence in bigger terrain. SH

Weather Forecast

Mainly cloudy and cool conditions over the next few days with only trace amounts of snow and light gusting moderate NW alpine winds.

Snowpack Summary

30-50cm of recent storm snow is bonding well to old surfaces. In the Lake Louise region, the Mar 2nd suncrust/facet layer can be found down 40-60 cm on S aspects, and the Feb 10 crust/facet layer is down 80-100cm on all aspects. Both are producing moderate to hard sudden failures with the potential to propagate. Fewer results on North aspects.

Avalanche Summary

No new avalanches observed today. There was one size 2.5 explosive controlled avalanche in the Lake Louise area yesterday which slid to ground on a N aspect in previously controlled terrain .

Confidence

Problems

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.

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.