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

Regions

South Columbia.

Incremental snowfall is out-pacing the snowpack's ability to adjust. Stay vigilant with simple terrain choices as the storm cycle 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 accumulation, moderate southwest wind, alpine temperature -7 C. 

Sunday: Cloudy, 5-10 cm of snow, moderate southwest wind, alpine high temperature -8 C. 

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

Tuesday: Cloudy, 20-30 cm of snow, moderate south wind, alpine high temperature -3 C.

Avalanche Summary

Widespread, large (size 2-2.5) natural, human, and explosive-triggered storm slab avalanches were reported across the region on Friday and Saturday. Avalanches were 30-60 cm deep and were reported on all aspects and elevations. Some of these were remotely-triggered (i.e. from a distance). 

Three notable persistent slab avalanches released naturally on east and northeast facing slopes above 2200 m in the southern part of the region on a crust/facet layer from late November buried 150 cm deep. These avalanches give clear evidence that the continual loading on this fundamentally weak snowpack structure remains a serious concern.

Snowpack Summary

60-120 cm of new snow has fallen throughout 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. The storm snow overlies a weak layer of feathery surface hoar and a hard melt-freeze crust on sun-exposed aspects, which has increased the reactivity of these slabs.

There are multiple weak layers buried around 80 to 200 cm deep, including two more surface hoar layers from December and weak faceted snow on a crust near the bottom of the snowpack from late November. It is possible that easier-to-trigger storm slab avalanches could step down to these deeper, persistent layers or that the weak layers could be human-triggered in areas 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.
  • Storm slabs in motion may step down to deeply buried weak layers resulting in very large avalanches.
  • Remote triggering is a concern, watch out for adjacent and overhead slopes.

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.