Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
Cold, northerly winds are redistributing the recent snow into potentially reactive windslabs. With cold temperatures windslabs will take longer then usual to stabilize and bond to the underlaying surfaces.
Be especially cautious at treeline elevations where the overlaying slab may sit on top of large feathery, surface hoar crystals.