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Avalanche Forecast

Archived

Nov 30th, 2021–Dec 1st, 2021

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

Regions

Yukon.

Reactive wind slabs at treeline and in the alpine may exist on all aspects due to changing winds. 

Confidence

Moderate -

Weather Forecast

An onshore flow will bring mostly cloudy skies, new snow, and moderate to strong mountain top wind. Tuesday’s easterly wind will switch back to the southwest. 

Wednesday: New snow 5-10 cm. Alpine temperatures -12 C to -15 C and ridgetop wind moderate from the southwest.

Thursday: Light snow in the morning 3-5 cm. Alpine temperatures -15 C. Ridgetop wind generally light from the southwest. 

Friday: Trace of new snow. Alpine temperature dipping to – 22 C. Ridgetop wind light from the northeast switching to the southeast later in the day.

Avalanche Summary

No recent reports of avalanche activity on Tuesday. 

Over the weekend, large natural avalanches (size 2 and 2.5) were on alpine lee features. A MIN report also noted a slab release size 2 above Bryant Lake.

Lots of whumpfing and cracking have been notified across the region and are most likely to be associated with early-season shallow snowpack and wind-affected snow.

Snowpack Summary

Up to 5 cm of new snow fell overnight Monday. On most aspects above the treeline, wind-affected snow exists showing signs of cracking, whumfing, and cross-loading. Wind slabs are present and potentially reactive to human triggers. 

Little information is available about a weak layer of facets over a crust reported lower in the snowpack. Snow depths are approximately 80 cm at treeline and 100-120 in the alpine.

Terrain and Travel

  • Wind slabs are most reactive during their formation.
  • Avoid freshly wind loaded terrain features.
  • Approach lee and cross-loaded slopes with caution.
  • Be especially cautious near rock outcroppings, on steep convexities and anywhere the snowpack feels thinner than average.

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.