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Avalanche Forecast

Archived

Dec 29th, 2020–Dec 30th, 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 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

North Columbia.

  

Recently formed storm slabs will be most reactive in wind affected areas a treeline and above. Be especially cautious as you transition into wind affected terrain.

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

  

TUESDAY NIGHT: Cloudy / Light, southwest ridgetop wind / alpine low temperature -14 / Freezing level valley bottom.

WEDNESDAY: Snow; 5-15 cm. / Moderate, southwest ridgetop wind / alpine high temperature -9 / Freezing level valley bottom.

THURSDAY: Cloudy with isolated flurries; 0-3 cm. / Light, west ridgetop wind / alpine high temperature -8 / Freezing level valley bottom.

FRIDAY: Snow; 5-10 cm. / Strong, southwest ridgetop wind / alpine high temperature -6 / Freezing level rising to 700 m.

Avalanche Summary

  

25-40 cm. of new snow since Christmas day has buried yet another weak layer of surface hoar that was widespread at treeline and below. Expect this new snow to become increasingly reactive to human triggers as it settles into a cohesive slab.

There have been numerous recent reports of dry loose avalanches(sluffs) running surprisingly fast and far below treeline.

 

Snowpack Summary

25-40 cm. of new snow since Christmas day has buried yet another weak layer of surface hoar that was widespread at treeline and below. Expect this new snow to become increasingly reactive to human triggers as it settles into a cohesive slab.

Lingering wind slabs formed last week may remain reactive on a variety of aspects due to shifting winds.

About one meter below the surface is the mid December surface hoar. This layer has recently been sensitive to human triggering.

Below that lies the early December persistent weak layer, it's about 80 to 140 cm below the surface. This weak layer is a mixed bag that often presents as surface hoar and facets sitting on top of a supportive crust. This is a nasty weak layer, when avalanches fail on it, they have been large and destructive. Smaller avalanches in motion may step-down to this layer resulting in very large and destructive avalanches. 

Terrain and Travel

  • Be especially cautious as you transition into wind affected terrain.
  • Uncertainty is best managed through conservative terrain choices at this time.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Avoid open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.
  • Storm slabs in motion may step down to deeper layers resulting in 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.