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Avalanche Forecast

Archived

Jan 4th, 2020–Jan 5th, 2020

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

Regions

North Columbia.

Continuing snowfall and wind is out-pacing the snowpack's ability to adjust. Stay vigilant with simple terrain choices as this pattern continues.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Saturday night: Cloudy, scattered flurries with 2-5 cm of accumulation, moderate to strong southwest wind, alpine temperature -8 C. 

Sunday: Cloudy, 5-15 cm of snow, moderate to strong southwest wind, alpine high temperature -8 C.

Monday: Mostly cloudy with 5-10 cm of snow, light southwest wind, alpine high temperature -7 C.

Tuesday: Cloudy, 20-30 cm of snow, light southeast wind, alpine high temperature -5 C.

Avalanche Summary

Widespread, large (size 2-3) natural and human-triggered storm slab avalanches were reported across the region on Saturday. These avalanches were 20-60 cm deep and were reported on all aspects and elevations. Some of these were remotely-triggered (i.e. from a distance).

A report of a larger (size 3.5) avalanche from nearby Glacier National Park indicates that the continual loading on more deeply buried weak layers remains a concern.

Snowpack Summary

60-100 cm of new snow has fallen over the past week creating a touchy storm slab problem. At high elevations, this snow has been redistributed by strong southwest winds, loading lee features near ridges and exacerbating reactivity. The storm snow overlies a weak layer of feathery surface hoar and a hard melt-freeze crust on sun-exposed aspects, also increasing the reactivity of these slabs.

There are a couple more deeply buried weak layers, including a surface hoar layer from mid-December buried 110 to 180 cm deep and a facet/crust layer from late November buried over 180 cm deep. There is lingering concern that easier-to-trigger storm slab avalanches could step down to these deeper, persistent layers or that these weak layers could be human-triggered in areas in the alpine where the snowpack is thin, rocky, or variable.

Terrain and Travel

  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Be alert to conditions that change with elevation and wind exposure.
  • Avoid freshly wind loaded terrain features.
  • Be aware of the potential for large avalanches due to the presence of buried weak layers.

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.