Regions
Sexten Dolomites, Latemar, Southern Adamello, Adamello - Presanella, Northern Brenta - Peller, Bondone and Stivo, Folgaria - Laverone, Southern Brenta, Southern Lagorai, Northern Lagorai, 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, Maddalene, Pine' - Mocheni Valley, 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, Primiero - Pale di S. Martino, Eastern Deferegger Alps, Prags Dolomites, Prealps, Schober Mountains, Cembra Valley, Lienzer Dolomites, Vallarsa, Western Nonsberg Alps, Fassa Valley, Sole, Pejo and Rabbi, Ledro Valley, Paganella, Marzola - Valsugana
AM
Danger level
PM
Danger level
Avalanche Problem
Wet snow above 2400m, N-NE-E-W-NW
The avalanche danger after a clear night will be low (level 1).
The Avalanche Warning Service currently has only a small amount of information that has been collected in the field. Wet avalanches during the day are the main danger. As a consequence of warming during the day and the solar radiation, the likelihood of wet avalanches being released will increase gradually. The avalanche prone locations are to be found in particular on steep west to north to east facing slopes above approximately 2400 m. In some places wet avalanches can release the saturated snowpack and can reach as far as areas without any snow cover. In the runout zone hardly any snow is lying.
Snowpack
dp 10: springtime scenario
Outgoing longwave radiation during the night will be good in some case. The surface of the snowpack will freeze to form a strong crust and will soften during the day. Individual weak layers exist deep in the old snowpack on steep shady slopes, especially above approximately 2800 m in areas where the snow cover is rather shallow. At low altitude no snow is lying.
Tendency
Increase in danger of wet avalanches as a consequence of warming during the day and solar radiation.