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Avalanche Forecast

Archived

Dec 4th, 2024–Dec 5th, 2024

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

Regions

South Columbia, Shuswap, Dogtooth, West Purcell, Badshot-Battle, Central Selkirk, Goat, Gold, North Okanagan, Retallack, Valhalla, Whatshan.

Lingering wind slabs may be reactive in leeward terrain features at higher elevations. If the inversion is strong, avoid snow that is becoming moist as it could produce a small avalanche.

Confidence

Low

Avalanche Summary

Wet loose avalanches up to (size 1) were seen from steep south-facing terrain at upper elevations. Additionally, few natural slab avalanches (size 2.5) were seen from steep southwest aspects. Reports indicate they were several days old. Below treeline a natural glide slab release (size 2) was also noted and several days old.

Wind slabs continue to linger in the region, with reports indicating they are stubborn to rider triggering.

Snowpack Summary

Surface conditions vary from wind affected snow in exposed terrain at higher elevations, and settling snow in sheltered areas. Surface hoar development is widespread and a crust has formed on steeper slopes exposed to the sun.

Buried surface hoar can be found 5 to 20 cm deep.

The mid snowpack is generally well settled, with an early November crust buried 50 to 100 cm deep. This layer is understood to be more notable in the Selkirk Mountains.

Snow depths at treeline are roughly 80 to 150 cm, and decrease rapidly at lower elevations.

Weather Summary

Wednesday Night:

Partly cloudy. 15 to 20 km/h west ridgetop winds. Treeline temperatures around -5 °C with an above-freezing layer bringing the alpine temperatures to 0 °C.

Thursday:

Valley cloud with sunny periods at treeline and above. 15 to 30 km/h west ridgetop wind. The above-freezing layer brings alpine temperatures around +1 °C to + 3 °C. Treeline and below temperatures near -2 °C.

Friday

Cloudy with snow 5 to 15 cm. 40 to 50 km/h southwest ridgetop wind. The above-freezing layer brings alpine temperatures around 0 °C. Treeline temperatures near -2 °C.

Saturday

Cloudy. New snow 10 to 25 cm. 15 to 35 km/h southwest ridgetop wind. Alpine temperatures near -3 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be careful with wind-loaded pockets, especially near ridge crests and rollovers.
  • Back off slopes as the surface becomes moist or wet with rising temperatures.
  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.

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.