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Avalanche Forecast

Archived

Mar 9th, 2022–Mar 10th, 2022

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

Regions

North Columbia.

 Recently formed wind slabs may remain reactive to human triggers on steep and/or convex slopes.

Cornices are very large in many areas. Cornice failures may trigger large avalanches on the slopes below.

Confidence

High -

Weather Forecast

WEDNESDAY NIGHT: Partly cloudy / Moderate northwest winds / Low of -20 / Freezing level surface.

THURSDAY: Increasing cloudiness / Light west wind / High of -7 / Freezing level surface.

FRIDAY: Cloudy with flurries; 3-5 cm / Moderate west wind / High of -5 / Freezing level rising to 1000 m.

SATURDAY: Snow; 10-20 cm / Strong southwest wind / High of -1 / Freezing level 1400 m.

Avalanche Summary

Several skier triggered wind slabs up to size 2 were reported on Tuesday.

Snowpack Summary

Recent west and northwest winds have formed wind slabs on lee features at treeline and above. These slabs may remain more reactive on south facing slopes where they are sitting on a slippery sun crust. Below the recent snow, there may be a layer of small surface hoar that is likely most pronounced on northerly aspects or sheltered locations.

Lower elevations have seen warm temperatures last week and have a melt freeze crust on the surface below 1600 m.

The late February weak layer combination of crust, facets and surface hoar is down 30-40cm deep, and has been reactive mostly on south facing slopes during periods of sun. 

Two persistent weak layers from mid February and late January are buried 50-120cm deep. No recent avalanches have been reported on these layers but they continue to produce the occasional notable result in snowpack tests.

The most likely triggers of these persistent weak layers are large triggers such as smaller avalanches in motion, cornices, or snowmobiles.

Terrain and Travel

  • Cornice failure may trigger large avalanches.
  • Minimize your exposure time below cornices.
  • Carefully evaluate steep lines for wind slabs.
  • Wind slabs may be poorly bonded to the underlying crust.
  • Use ridges or ribs to avoid areas of wind loaded snow.

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.