Persistent weak layers
- Above 1,800 m
- Size
- 3
Stability: poor · Frequency: some
New snow and wind slabs represent the main danger.
Stability: poor · Frequency: some
Stability: poor · Frequency: some
Stability: fair · Frequency: few
New snow and wind slabs represent the main danger.
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 starting zones where no previous releases have taken place and on wind-loaded slopes medium-sized and large avalanches are possible as a consequence of new snow and wind. The new snow and wind slabs can be released easily, even by a single winter sport participant,. Whumpfing sounds and natural avalanches serve as an alarm sign. Remotely triggered avalanches are possible. Caution is to be exercised in particular in the regions exposed to heavier precipitation. Isolated very large dry avalanches are possible here. Backcountry touring and other off-piste activities call for defensive route selection.
The sometimes strong wind has transported some snow. This situation gave rise to unfavourable bonding of the snowpack over a wide area. The new snow and wind slabs are prone to triggering. This applies especially at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. New snow and wind slabs are lying on a weakly bonded old snowpack, in particular on shady slopes. Large-grained weak layers exist in the snowpack on shady slopes.
Bulletin data: ARPA Lombardia (via EAWS / avalanche.report)