Wind slab
- Above 2,000 m
- Size
- 3
Stability: poor · Frequency: some
Wind slabs and wet snow represent the main danger. Weak layers in the old snowpack necessitate defensive route selection.
Stability: poor · Frequency: some
Stability: poor · Frequency: some
Stability: poor · Frequency: few
Wind slabs and wet snow represent the main danger. Weak layers in the old snowpack necessitate defensive route selection.
The avalanche prone locations are covered with new snow and are difficult to recognise, in particular in gullies and bowls, and behind abrupt changes in the terrain. In particular in east to south to west facing aspects and below approximately 2300 m medium-sized and large avalanches are possible as a consequence of warming during the day and solar radiation. Weak layers exist in the snowpack in shady places that are protected from the wind. Dry avalanches can be released, mostly by large loads and reach large size in isolated cases.
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.
Bulletin data: ARPA Lombardia (via EAWS / avalanche.report)