Wind slab
- Above 2,200 m
- Size
- 3
Stability: fair · Frequency: few
Wind slabs and wet snow represent the main danger. As a consequence of a strong wind, easily released wind slabs formed in particular adjacent to ridgelines on south, east and west facing slopes.
Stability: fair · Frequency: few
Stability: poor · Frequency: few
Stability: fair · Frequency: few
Large-grained weak layers exist in the snowpack on shady slopes. This applies especially at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example.
Wind slabs and wet snow represent the main danger. As a consequence of a strong wind, easily released wind slabs formed in particular adjacent to ridgelines on south, east and west facing slopes.
The avalanche prone locations are clearly recognisable to the trained eye, especially adjacent to ridgelines, in particular in the central part of the main Alpine ridge. Weak layers exist in the snowpack in shady places that are protected from the wind. Dry avalanches can still be released, mostly by large loads.
Bulletin data: ARPA Lombardia (via EAWS / avalanche.report)