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 and Persistent Slabs.
JSmith,
Avalanche Canada
Cornices are very large in many areas. Cornice failures may trigger large avalanches on the slopes below.
Large skier triggered persistent slab avalanches have surprised riders in the southern Selkirk mountains over the past week.
Summary
Confidence
High -
Weather Forecast
WEDNESDAY NIGHT: Mostly clear / Moderate northwest winds / Low of -20 / Freezing level surface.
THURSDAY: Mix of sun and cloud / Light northwest wind / High of -6 / Freezing level valley bottom.
FRIDAY: Mostly cloudy / Light northwest wind / High of -3 / Freezing level rising to 1100 m.
SATURDAY: Snow; 10-20 cm / Strong southwest wind / High of 0 / Freezing level 1500 m.
Avalanche Summary
Numerous skier triggered, size 1 wind slabs on primarily north and east aspects on Tuesday. Additionally, a size 2 natural cornice failure triggered a large (size 2.5) wind slab.
Over the past week we have seen the buried weak layers of surface hoar and crust from mid February and late January produce very large persistent slab avalanches up to size 3. Activity has been concentrated in the Valhalla, Goat, and Kokanee Ranges typically on north through southeast facing slopes at treeline elevations.
- Multiple size 2-3 avalanches were remotely triggered from ridgeline features on Friday and Saturday, up to 90cm deep.Â
- A natural size 2 was triggered by solar input in the Valhallas on Friday.Â
- On Friday snowmobile triggered size 2 occurred near Slocan. Read the MIN report here for full details.Â
The most likely triggers of these persistent slabs are large triggers such as smaller avalanches in motion, cornices, or snowmobiles.
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 1800 m.
The late February persistent weak layer combination of crust, facets and surface hoar is buried up to 50cm deep, and has been reactive mostly on south facing slopes during periods of sun.Â
Two additional persistent weak layers sit 50-120 cm deep, from mid February and late January. They both consist of surface hoar and/or melt-freeze crusts. Recent trends indicate these layers have been more reactive in southern Selkirks around the Valhalla, Kokanee, and Goat Ranges. Several natural and human triggered avalanches have been produced on these layers in the last week. See the Avalanche Summary for full details.
Terrain and Travel
- Cornice failure may trigger large avalanches.
- Minimize your exposure time below cornices.
- Carefully evaluate steep lines for wind slabs.
- Be aware of the potential for large avalanches due to the presence of a persistent slab.
- Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
Problems
Wind Slabs
Recently formed wind slabs may remain reactive to human triggers in specific 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
Persistent Slabs
Persistent weak layers of surface hoar and/or crust can be found 40 to 120 cm deep.
The problem is most likely found in the southern part of the Selkirks (e.g. Valhalla, Goat and Kokanee ranges), especially on open convex slopes at treeline elevations.
This problem exists on all aspects, however increased reactivity has been noted on northeast through southeast facing slopes.
Conservative terrain choices and disciplined decision making is required in areas where these persistent slabs remain reactive.
Aspects: All aspects.
Elevations: Treeline.
Likelihood
Expected Size
Valid until: Mar 10th, 2022 4:00PM
