Storm Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2.5
20-30 cm of recent storm snow has formed reactive storm slabs at all elevations. The new snow slab becomes stiffer with the settlement of the snow and rising temperatures. A failure in the weak layer underneath the slab might propagate wider than expected resulting in larger avalanches. The storm slabs are particularly reactive where they overlie surface hoar in sheltered areas at and below treeline.
The new snow is redistributed by moderate to strong southwest wind and forms fresh wind slabs on lee terrain features at higher elevations.
Cornices are growing larger and becoming more fragile.