Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Once the rain transitions back to snow, transition your attention to dry snow avalanches and slabs that form as the wind loads lee slopes. Wind slabs may not become a problem until late morning or the afternoon, but once you have several inches or more of fresh snow in your terrain, anticipate shallow slabs on wind-loaded slopes. Actively blowing and drifting snow indicates the growing instability in your terrain. Cracking indicates you are moving onto a slab that you can trigger once it becomes sufficiently thick. If you can't see the rain rill texture in the terrain, wind slabs have likely formed and are large enough to produce an avalanche. If you suspect a problem, steer around wind-loaded slopes steeper than 35 degrees.
Example: Wind slab below corniced ridgeline.
Photo: Jeff Zimmerman