Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible - Likely
- Size
- 1–2
Recent southwest winds and new snow have formed wind slabs in lee terrain features. Winds are expected to transition to a west-northwesterly flow, which may encourage "reverse loading" building fresh wind slabs on more south and easterly slopes. Steep, convex slopes below alpine ridge tops are the most likely places to trigger these slabs.