Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Yesterday afternoon and last night, increased westerly winds caused some drifting at higher elevations, forming a fresh generation of shallow wind slabs below corniced ridges or in cross-loaded terrain features. Monitor for evidence of recent drifting, such as thicker, harder pillows of snow to identify features of concern. You can avoid wind slabs by traveling in wind-sheltered terrain.
A shallow Wind Slab from earlier this week below a leeward ridgeline.