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Avalanche Forecast

Archived

Dec 5th, 2020–Dec 7th, 2020

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

Regions

Yukon.

  

Continued snow with strong, southwest winds will keep the hazard elevated through the weekend. Choose conservative terrain as human triggered avalanches remain likely, especially in wind loaded areas.

Confidence

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

Weather Forecast

  

SATURDAY NIGHT: Snow; 5-10 cm. / Strong, southwest ridgetop wind / alpine low temperature -10 / Freezing level valley bottom.

SUNDAY: Snow; 5-10 cm. / Strong, southwest ridgetop wind / alpine high temperature -8 / Freezing level valley bottom.

MONDAY: Snow; 10-15 cm. / Moderate, southwest ridgetop wind / alpine high temperature -7 / Freezing level valley bottom.

TUESDAY: Cloudy with isolated flurries; 0-3 cm. / Moderate, southwest ridgetop wind / alpine high temperature -7 / Freezing level valley bottom.

Avalanche Summary

A widespread natural avalanche cycle with numerous avalanches up to size 3 was reported to have occurred in the White Pass area, mostly during the height of the storm (Monday-Wednesday) Check out this MIN report detailing these observations.

With more snow and wind on the way, it is expected that avalanches will remain likely to human trigger over the weekend, especially in wind loaded areas.

Snowpack Summary

  

Continued snow with strong, southwest winds are forecast through the weekend.

The White Pass area received over 100 cm of new snow earlier in the week with strong southwest winds. Total snowpack depth is around 175 cm in sheltered areas around White Pass.

In drier areas such as the Wheaton Valley, total snowpack depths are likely in the 50-100 cm range and are probably quite variable due to wind transport. The base of the snowpack in this area may consist of some weak, sugary facets

 Both storm slabs and wind slabs are likely widespread in the region and may be easily triggered by humans. Storm slabs may be more prevalent in the White Pass area, while wind slabs may be more prominent in areas like the Wheaton Valley.

Terrain and Travel

  • Watch for fresh storm slabs building throughout the day.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Recent new snow may be hiding windslabs that were easily visible before the snow fell.
  • Avoid lee and cross-loaded terrain.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.