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Avalanche Forecast

Archived

Dec 14th, 2021–Dec 15th, 2021

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

Regions

Yukon.

Wind slabs are likely getting more difficult to trigger, but we'd still suggest avoiding steep south facing terrain where wind slabs are probably thick and hard. If you are getting out, please submit to the Mountain Information Network and let us know what you're seeing.

Confidence

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

Weather Forecast

Still cold for the foreseeable future.

TUESDAY NIGHT: Overnight low temperature around -28, light variable wind, no snow expected.

WEDNESDAY: Scattered cloud cover, daytime high temperature around -24, wind begins to pick up midday mainly out of the northwest, could be strong to extreme Wednesday night at upper elevations, no significant snowfall expected during the day or night. 

THURSDAY: Clear skies, daytime high temperature around -28, strong northwest wind at upper elevations, no snow expected during the day, a few cm possible Thursday night.

FRIDAY: Scattered cloud cover, daytime high temperature around -18, moderate southwest wind at upper elevations, a few cm of snow possible.

Avalanche Summary

Several avalanches to size 1.5 were observed on south facing aspects Monday, the result of last weekend's strong north wind event.

Explosive control earlier in the month produced many large avalanches that failed on the weak sugary crystals at the bottom of the snowpack. These avalanches ran full path.

On December 1, a size 2.5 avalanche was remotely triggered by a recreational group on Log Cabin. This avalanche likely failed on the weak, sugary snow at the bottom of the snowpack. 

Triggering the deep layer (see the December 1 avalanche described above) is most likely to occur in shallow areas or where the snowpack variable in depth with a mix of shallow and deep zones. 

Snowpack Summary

Northerly winds have gotten into almost all the terrain of the White Pass, even down into the trees at lower elevations which has resulted in quite a bit of wind slab development on south facing features. Big thanks to the party who submitted this MIN on Sunday! Lots of shooting cracks were observed as they were out in the Fraser Chutes Sunday. It is getting pretty hard to find snow that is not wind effected.

The middle snowpack is supportive to travel but snow depth still varies greatly with aspect and elevation. 

A layer of weak, sugary snow at the base of the snowpack has been observed in most areas. This layer was reactive earlier in December, and it might still be possible to trigger this deeply buried layer in shallow snowpack areas or if a cornice fall or surface avalanche impacts a slope. If triggered, this basal layer could produce large avalanches. This sugary layer will likely become weaker in the coming days with cold temperatures potentially making it increasingly sensitive to triggering.

Terrain and Travel

  • Watch for areas of hard wind slab on alpine features.
  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.
  • Be aware of the potential for large avalanches due to the presence of a deep persistent slab.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.