Sole, Pejo and Rabbi

As a consequence of a strong wind, sometimes avalanche prone wind slabs formed in the last few days in particular adjacent to ridgelines in all aspects.

As a consequence of a strong wind, sometimes avalanche prone wind slabs formed in the last few days in particular adjacent to ridgelines in all aspects.

Weak layers in the old snowpack can still be released by winter sport participants. Such avalanche prone locations are to be found in particular on very steep shady slopes above approximately 2500 m. In particular, however, the wind slabs of the last few days adjacent to ridgelines and in gullies and bowls are capable of being triggered in some locations. (--), caution is to be exercised on wind-loaded slopes in particular above approximately 2500 m, and adjacent to ridgelines in all aspects. Avalanches can also penetrate down to the ground and reach quite a large size. This applies on very steep shady slopes in particular at high altitude.

Avalanche prone weak layers exist in the old snowpack especially on little used west, north and east facing slopes. This applies on shady slopes above approximately 2500 m. As a consequence of the sometimes strong wind the wind slabs have increased in size. The snowpack will be generally subject to considerable local variations. Below the tree line a little snow is lying.

The avalanche danger will persist.