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Avalanche Forecast

Archived

Mar 15th, 2015–Mar 16th, 2015

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

Regions

Kootenay Boundary.

Forecast danger ratings are focused on the south of the region where heavy snowfall is expected. If you see lower snowfall amounts, these danger ratings may be a bit high.

Confidence

Fair - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

Snow above 1200 metres combined with moderate southwest winds tonight and Monday morning. 15-30 cm of snow is forecast for alpine elevations by late Monday morning. Monday should be cloudy with some lingering flurries and light easterly winds. Freezing levels should drop down to about 1000 metres by Tuesday morning. Mostly sunny with light winds on Tuesday and freezing levels rising up to about 1800 metres. Cloudy on Wednesday with moderate southwest winds and light precipitation.

Avalanche Summary

No new avalanches reported. I expect new snow and wind to create fresh windslabs that may be very touchy to human triggers.

Snowpack Summary

Forecast heavy precipitation is expected to fall as snow above about 1200 metres. New snow and wind are expected to develop new storm slabs above the rain soaked snowpack. Heavy rain on Saturday soaked the snowpack up to ridge tops. Strong southwest winds combined with new snow at higher alpine elevations may have developed new wind slabs that are easy to trigger, and may allow for long propagations where they are sitting on a crust/facet combination. The most prominent feature in the snowpack is the thick late-February crust, down 5-20 cm before the ongoing storm. Limited reports suggest this crust is breaking down in some areas, while it remains supportive all the way to ridge crest in other spots. Deeply buried persistent weak layers still exist in the snowpack. These layers have not been reactive lately, however the extremes of warm weather followed by heavy loading due to rain then followed by snow, make it difficult to assess how the snowpack will respond.

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.