Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
Light snowfall and gusty southwest winds drifted snow into thin slabs at the tail end of the Atmospheric River. They will be larger and thicker just downwind of the higher-elevation ridgelines, saddles, and summits.
These features will have a dune-shaped appearance and may sound hollow. In some areas, they may be sufficiently dense to support the weight of a rider or a machine. The recent warm weather has likely strengthened these features, but if you notice cracks shooting away from your skis or machine, you have found a sensitive slab.
Upper-elevation slopes that have not been affected by wind will provide a softer, safer experience.