Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–2
Winds have formed reactive slabs in lee features at upper elevations. Where the new snow overlies surface hoar (or a crust) a poor bond has been noted, and reactively will increase as winds encourage cohesion and slab properties. Dig down to investigate developing slabs in the upper snowpack and a poor bond to older surfaces. The problem is more likely found in northern parts of the region, in areas that have received the higher amounts of incremental snowfall (e.g. Golden).