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