Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1.5–2.5
20 cm of accumulated snow and strong northwest winds may have formed a wind slab over a supportive melt-freeze crust, which may become more reactive as temperatures rise throughout the day and new snow settles into a cohesive slab.