Avalanche Forecast
Issued: Mar 9th, 2022 4:00PM
The alpine rating is , the treeline rating is , and the below treeline rating is Known problems include Wind Slabs.
JSmith,
Avalanche Canada
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.
Summary
Confidence
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
Recently formed wind slabs may remain active to human triggers in isolated locations; especially where they are sitting on a slippery sun crust.
Cornices are very large in many areas. Cornice failures may trigger large avalanches on the slopes below.
Aspects: North, North East, East, South East, South.
Elevations: Alpine.
Likelihood
Expected Size
Valid until: Mar 10th, 2022 4:00PM
