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Avalanche Forecast

Archived

Jan 8th, 2023–Jan 9th, 2023

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

Regions

Yukon, Tutshi, Wheaton, White Pass East, White Pass West.

Assess for wind slabs in steep terrain.

Confidence

Moderate

Avalanche Summary

We haven't received reports of recent avalanches. Looking forward, isolated pockets of wind slabs could be triggered by riders in steep lee terrain features.

Snowpack Summary

5 to 10 cm of soft snow from the weekend overlies a settled snowpack. Southerly wind may have formed pockets of wind slabs in lee terrain features.

Snow depths at White Pass are around 100 cm in sheltered areas and 200 cm on wind-loaded slopes.

Weather Summary

Sunday night

Cloudy with no precipitation, 5 km/h west wind, alpine temperature -6 °C.

Monday

Cloudy with no precipitation, 5 km/h south wind, alpine temperature -8 °C.

Tuesday

Mix of sun and cloud, 10 to 20 km/h southeast wind, alpine temperature -10 C.

Wednesday

Mostly sunny, 10 km/h southwest wind, alpine temperature -10 C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Use ridges or ribs to avoid areas of wind loaded snow.
  • The best and safest riding will be on slopes that have soft snow without any slab properties.

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.