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Avalanche Forecast

Archived

Jan 12th, 2014–Jan 13th, 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 unlikely, human triggered possible.
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

Kootenay Boundary.

Confidence

Fair - Intensity of incoming weather systems is uncertain

Weather Forecast

Tonight and Monday: Moderate precipitation is expected tonight with extreme W winds. Freezing levels are expected to rise to 100 m on Monday. Tuesday: An upper ridge is building over the region which will give the storm pattern a break. Trace accumulations, a mix of sun and cloud, strong W winds and freezing levels rising to 2000 m. Wednesday: The ridge brings dry, clear and warm temperatures over the Southern part of the province with strong winds from the NW.

Avalanche Summary

There was a natural avalanche cycle yesterday up to size 2.5 from all aspects at all elevations but mostly on N and NE aspects. Some are suspected to have run on the early January surface hoar layer. There was also some small avalanches triggered by skiers without involvement on East aspects.

Snowpack Summary

Accumulations forecasted tonight, strong W winds and rising freezing levels is keeping avalanche conditions dangerous for tomorrow. New windslabs lee of wind will take time to bond to the underlying surfaces, such as older windslabs in the alpine and previous storm snow in sheltered areas. The storm snow is expected to have to potential to sluff in steep sheltered terrain. Under the ~40 cm of recent storm snow, a surface hoar layer is present at treeline and below treeline and is sitting on a sun crust on S facing aspects. Some avalanches are suspected to have stepped down to this layer during the last avalanche cycle. The end of November facet/crust or surface hoar layer down 90 cm (or 50 cm where snowpack is very thin) and the depth hoar or basal facetting are still a concern. The facet/crust layer is most reactive on S and SE aspects slopes in the South-Eastern part of the region and seems to be more problematic on N and NE aspects in the central-Southern part of the region where the surface hoar was preserved.

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.