Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Cold, northerly winds are redistributing new snow into potentially reactive windslabs. With cold temperatures windslabs will take longer then usual to stabilize and bond to the underlaying, hard surfaces.
Be especially cautious at treeline elevations where the overlaying slab may sit on top of large feathery, surface hoar crystals.