Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible
- Taille
- 1–1.5
New snow may form isolated pockets of unstable wind slabs in the alpine.
Be careful around cornices and watch for new snow forming isolated wind slabs in the alpine.
New snow may form isolated pockets of unstable wind slabs in the alpine.
Minimize your exposure below cornices. Cornice falls are dangerous on their own and can possibly trigger avalanches on slopes below.
A cold front crossing the region on Thursday will bring a shift to cooler stormy weather.
WEDNESDAY NIGHT: Increasing clouds, 40 km/h northwest wind, freezing level drops to 1200 m with treeline temperatures dropping to -4 C.
THURSDAY: Cloudy with light flurries bringing up to 5 cm of snow across the region, light northeast wind, freezing level climbs to 1600 m with treeline temperatures around -3 C.
FRIDAY: Cloudy with scattered flurries bringing 5-15 cm of new snow, flurries easing in intensity throughout the day, light southwest wind, freezing level climbs to 1800 m with treeline temperatures around -2 C.
SATURDAY: Cloudy with scattered flurries bringing another 5-10 cm of snow, light southeast wind, freezing level climbs to 1800 m with treeline temperatures around -2 C.
Warm temperatures over the past week resulted in widespread wet avalanche activity, primarily on sun-exposed slopes. Most of the activity was size 1-2 wet loose avalanches, but a few larger and destructive wet slab avalanches were reported (near the Bugaboos on Saturday and near Golden on Monday). Some large cornice falls were also observed.
The cooling trend will make wet avalanches problems less likely in the coming days, making isolated wind slabs and cornice falls the primary concern.
A dusting of new snow will sit above a thick surface crust. The upper snowpack has been undergoing a daily melt-freeze cycle, so with the cooling temperatures a hard crust will form everywhere except in high north-facing terrain where there still may be dry snow above roughly 2300 m. We suspect older weak layers have gone inactive as the weather patterns over the past month have been favourable for strengthening the snowpack.