Pre Alps

Avalanche danger is low. On very steep grass-covered slopes, mostly small glide-snow avalanches can trigger naturally.

The snowpack was able to settle and consolidate somewhat due to higher temperatures and solar radiation. Particularly on shady slopes in the uppermost part of the snowpack there are weak layers evident which can easily be triggered. During the course of the day, superficially melt-freeze encrusted layers are becoming moist on steep sunny slopes, often wind crusts. On steep sunny slopes a melt-freeze crust is evident. Encrusted snowpack surfaces moisten during the day.

Tranquil mountain weather without perturbances from early until late. In the Rhine Valley there is a sea of fog, but the sky is cloudless. Hardly any wind, and not cold. At 2000m: +1 degree. Light winds from northerly directions at high altitudes.

Avalanche danger levels are not expected to change significantly.