Border Graie Alps

As a consequence of the sometimes storm force wind the avalanche prone locations will become more prevalent.

The avalanche danger will persist.

As a consequence of the sometimes storm force wind the avalanche prone locations will become more prevalent.

As a consequence of the sometimes storm force foehn wind the avalanche prone locations will become more prevalent. In particular on steep slopes and in gullies and bowls, and behind abrupt changes in the terrain medium-sized slab avalanches are possible. Avalanches can be released, even by small loads in isolated cases. Between approximately 2400 and 3000 m the avalanche prone locations are more prevalent.

As a consequence of the wind, the snow drift accumulations have increased in size. Snow depths vary greatly at high altitude, depending on the infuence of the wind. Sunshine and high temperatures gave rise to consolidation of the snowpack at low and intermediate altitudes. At low and intermediate altitudes only a little snow is lying.