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Avalanche Forecast

Archived

Jan 14th, 2015–Jan 15th, 2015

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

Regions

Glacier.

Avalanche activity has decreased, but the Dec 17 surface hoar continues to surprise people. Keep this layer in mind as you choose objectives and plan your day.

Weather Forecast

Today should be a mix of sun and cloud, with an alpine high of -1 and light SW winds. On Thursday an incoming system will bring increasing cloud and isolated flurries later in the day. Through Friday we may see up to 15cm of snow with strong and gusty westerly winds which will amplify the new snow depth over the surface hoar that is growing now.

Snowpack Summary

A widespread new surface hoar layer is growing to mountain top. There is sun crust up to 2cm thick is present on steep solar aspects. A cohesive slab sits over the Dec 17 surface hoar, which is down 60cm-100cm. Crust/facet layers are present just below the Dec 17 layer with varying thicknesses depending on aspect and elevation.

Avalanche Summary

Sporadic avalanche activity continues. Small, loose solar triggered avalanches have been observed daily and there were two size 2's from North aspects yesterday. Outside the park a skier was caught in a size 2 when the Dec 17 failed on an unsupported roll. On the weekend a size 2 was ski cut on a moraine which failed on the Dec 17 surface hoar.

Confidence

Intensity of incoming weather systems is uncertain

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.