Regions
Sexten Dolomites, Allgäu Alps, Eastern Lechtal Alps - Ammergau Alps, Mieming Mountains, Karwendel Mountains, Brandenberg Alps, Wilder Kaiser Mountains - Waidring Alps, Western Lechtal Alps, Central Lechtal Alps, Grieskogel Mountains, Val Müstair Alps, Western Verwall Mountains, Langtaufers, Eastern Verwall Mountains, Schnals Ridge, Silvretta, Southern Stubai Alps, Samnaun Mountains, Southern Zillertal Alps and High Tauern, Northern Oetz and Stubai Alps, Saldurn-Mastaun Ridge, Western Tuxer Alps, Texel Mountains, Eastern Tuxer Alps, Sarntal Alps, Western Kitzbühel Alps, Western Pfunderer Mountains, Eastern Kitzbühel Alps, Glockturm Range, Eastern Pfunderer Mountains, Durreck Range, Weißkugel Range, Western Rieserferner Mountains, Gurgler Range, Western Deferegger Alps, Central Stubai Alps, Ortler Range, Northern Zillertal Alps, Ulten Valley, Venediger Range, Eastern Nonsberger Alps, Eastern Rieserferner Mountains, Northern Dolomites of Fiemme, Glockner Range, Gröden Dolomites, Eastern Deferegger Alps, Prags Dolomites, Schober Mountains, Lienzer Dolomites
Danger level
A generally favourable avalanche situation will prevail.
The Avalanche Warning Service currently has only a small amount of information that has been collected in the field.
The fresh and somewhat older wind slabs represent the main danger, in particular at high altitudes and in high Alpine regions. Wind slabs can in very isolated cases be released, in particular by large loads, especially on very steep shady slopes above approximately 2400 m. Mostly the avalanches are small.
Intermediate altitudes: As a consequence of warming during the day and solar radiation there will be only a slight increase in the danger of gliding avalanches and moist snow slides, in particular on steep sunny slopes.
Snowpack
Very steep shady slopes: The wind slabs are lying on soft layers. In very isolated cases weak layers exist in the old snowpack, in particular on steep, little used shady slopes above approximately 2200 m.
At low altitude no snow is lying.
Tendency
Gradual increase in avalanche danger as a consequence of the fresh snow, in particular in the north.