Regions
Sexten Dolomites, 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, 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, Allgäu Alps, Ulten Valley, Venediger Range, Eastern Lechtal Alps - Ammergau Alps, Eastern Nonsberger Alps, Mieming Mountains, Eastern Rieserferner Mountains, Northern Dolomites of Fiemme, Karwendel Mountains, Glockner Range, Gröden Dolomites, Eastern Deferegger Alps, Prags Dolomites, Schober Mountains, Lienzer Dolomites, Western Lechtal Alps, Central Lechtal Alps, Grieskogel Mountains
AM
Danger level
PM
Danger level
Avalanche Problem
Gliding snow above 2600m above 1800m, E-SE-S-SW-W
Wet snow above 2800m, E-SE-S-SW-W
Slight increase in avalanche danger as a consequence of warming during the day and solar radiation. At low and intermediate altitudes hardly any snow is lying.
The Avalanche Warning Service currently has only a small amount of information that has been collected in the field.
Early and late morning: Low avalanche danger will prevail.
Midday and afternoon: Slight increase in avalanche danger as a consequence of warming during the day and solar radiation. Gliding avalanches and wet snow slides are the main danger. The avalanche prone locations are to be found in particular on very steep sunny slopes below approximately 2800 m, but in isolated cases also on extremely steep shady slopes below approximately 2800 m.
In addition a low (level 1) danger of dry slab avalanches exists. This applies in particular on extremely steep shady slopes above approximately 2400 m. The avalanches are rather small and can be released by large loads.
Snowpack
dp 2: gliding snow
dp 10: springtime scenario
The surface of the snowpack has frozen to form a strong crust will soften earlier than the day before. This applies in particular on sunny slopes.
In very isolated cases weak layers exist in the old snowpack on shady slopes, especially above approximately 2400 m in areas where the snow cover is rather shallow.
At intermediate altitudes hardly any snow is lying. At low altitude no snow is lying.
Tendency
Increase in danger of gliding avalanches and snow slides as a consequence of warming during the day and solar radiation.