Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind loading may have formed unstable slabs on lee terrain features.
Triggering avalanches is possible on alpine slopes due to wind slabs and a buried weak layer.
Wind loading may have formed unstable slabs on lee terrain features.
A 50 to 100 cm deep weak layer from early December may be possible to trigger on steep slopes with shallow rocks.
No avalanches have been reported since the weekend.
On Sunday a rider triggered a large (size 2.5) slab avalanche on a southeast alpine slope. The slab ranged from 20 to 100 cm deep with wind loading variability. The slab may have released on the persistent weak layer described in the Snowpack Summary.
Surface conditions are highly variable, with small amounts of snow and strong winds forming pockets of wind slabs. Crusts have been reported on south-facing slopes, and surface hoar has been observed at lower elevations.
A weak layer of facets and crust from early December is buried approximately 50 to 100 cm deep. This layer likely contributed to avalanches last weekend but should be less reactive under current conditions, primarily posing a concern on steep rocky slopes.
Wednesday Night
Mostly cloudy with up to 5 cm of snow. 40 to 70 km/h west ridgetop wind. Treeline temperature -8 °C.
Thursday
Sunny. 10 km/h southeast ridgetop wind. Treeline temperature -12 °C.
Friday
Mostly cloudy with 5 to 10 cm of snow. 50 km/h southeast ridgetop wind. Treeline temperature -12 °C.
Saturday
Mix of sun and cloud. 30 km/h northeast ridgetop wind. Treeline temperature -17 °C.
More details can be found in the Mountain Weather Forecast.