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Avalanche Forecast

Archived

Jan 7th, 2020–Jan 8th, 2020

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

Regions

North Columbia.

A rapid, critical load has been added to the snowpack. Touchy conditions with high consequences will be widespread on Wednesday. Travel in avalanche terrain is not recommended.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

Tuesday night: Cloudy, 20-30 cm of snow, moderate southwest wind, alpine temperature -4 C.

Wednesday: Cloudy, snow tapering by noon with 5-10 cm of accumulation, moderate west wind, alpine temperature -9 C.

Thursday: Partly cloudy, isolated flurries with trace accumulations, light west wind, alpine high temperature -10 C.

Friday: Cloudy, 5-15 cm of snow, moderate south wind, alpine high temperature -10 C. 

Avalanche Summary

There have been many reports of large (size 2-2.5) avalanches from both natural and human triggers on a variety of aspects and elevations releasing on surface hoar layers formed in late December. These avalanches have been breaking 60-90 cm deep. Several of them have been remote-triggered.

As the new snow settles, storm slab avalanches are likely to be triggered and have the potential to step down to these deeper layers, forming very large and destructive avalanches.

Snowpack Summary

Up to 60 cm of new snow is forecast to accumulate by Wednesday afternoon with moderate to strong southwest wind. This will form a new storm slab problem that will need to be managed conservatively. Expect areas where the snow is being drifted by wind to be more reactive. 

Two layers of surface hoar from late December are now buried 60-120 cm deep. These layers continue to produce large avalanches across aspects and elevations. Small avalanches in the new snow have the potential to step-down to these persistent weak layers.

Terrain and Travel

  • Only the most simple non-avalanche terrain free of overhead hazard is appropriate at this time.
  • Be careful to keep storm day fever from luring you out into bigger terrain features.
  • If triggered, storm slabs in-motion may step down to deeper layers and result in very large avalanches.

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.