2025-03-27T16:00:00Z 2025-03-27T16:00:00Z 2025-03-28T16:00:00Z false Glockner Range Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Gurgler Range Central Stubai Alps Northern Zillertal Alps Venediger Range Lasörling Range Gröden Dolomites Lüsner Mountains Sexten Dolomites Upper Ahr Valley Southern Zillertal Alps Pfitsch Southern Sesvenna Group Schnals Ridge Northern Sesvenna Group Saldurn-Mastaun Ridge Hirzer Range Western Pfunderer Mountains Mount Saint Jakob Range Eastern Pfunderer Mountains Ratschings Durreck Range Langtaufers Rieserferner Mountains Southern Stubai Alps Western Deferegger Alps Ortler Range Ulten Valley Planeil Mountains Prags Dolomites Upper Passeier Valley Texel Mountains low 2200 earlier moderate 2200 earlier moderate later persistent_weak_layers 2200 NE W NW N E earlier poor few 2 slab wet_snow 2600 W SE SW NE N E S NW later poor some 2 loose persistent_weak_layers 2200 W NE N E NW later poor few 2 slab Increase in danger of wet avalanches as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution. An increasing number of small and medium-sized wet and gliding avalanches are possible as a consequence of warming during the day and solar radiation. This applies in particular on steep north and east facing slopes below approximately 2200 m, and elsewhere below approximately 2600 m. Weak layers in the old snowpack can still be released in isolated cases by individual winter sport participants. The avalanche prone locations are to be found in particular on steep, little used west, north and east facing slopes above approximately 2200 m. Mostly avalanches are medium-sized. In isolated cases avalanches can also release deeper layers of the snowpack and reach large size. In addition the mostly small wind slabs should be taken into account, in particular on very steep shady slopes adjacent to ridgelines in high Alpine regions. Restraint should be exercised because avalanches can sweep people along and give rise to falls. The surface of the snowpack will freeze to form a strong crust. Sunshine and high temperatures will give rise as the day progresses to increasing softening of the snowpack. Avalanche prone weak layers exist in the old snowpack especially on little used west, north and east facing slopes. The mostly small wind slabs are lying on soft layers in particular on very steep shady slopes in high Alpine regions. The snowpack will be generally subject to considerable local variations. Below the tree line only a little snow is now lying. The surface of the snowpack will cool hardly at all during the overcast night. Some snow will fall in some regions, in particular on the Main Alpine Ridge and in the High Tauern. steady 2025-03-28T16:00:00Z 2025-03-29T16:00:00Z 2025-03-28 DP10 DP5 2025-03-27T16:00:00Z 2025-03-27T16:00:00Z 2025-03-28T16:00:00Z false Brandenberg Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps Eastern Karwendel Mountains Central Kitzbühel Alps Western Kitzbühel Alps low earlier moderate later wet_snow S W SE SW E later poor some 2 loose As a consequence of warming during the day and solar radiation there will be only a slight increase in the danger of wet avalanches. In particular on extremely steep sunny slopes individual small and, in isolated cases, medium-sized wet loose snow avalanches are possible as a consequence of warming during the day and solar radiation. In addition individual gliding avalanches are possible. This applies in particular in the regions with a lot of snow. The surface of the snowpack will freeze to form a strong crust and will soften during the day. The snowpack will be generally subject to considerable local variations. Below the tree line only a little snow is now lying. The surface of the snowpack will cool hardly at all during the overcast night. Down to 1500 m snow will fall over a wide area. steady 2025-03-28T16:00:00Z 2025-03-29T16:00:00Z 2025-03-28 DP10 2025-03-27T16:00:00Z 2025-03-27T16:00:00Z 2025-03-28T16:00:00Z false Eastern Lechtal Alps Ammergau Alps Kauner Ridge Weißkugel Range Western Verwall Mountains Eastern Verwall Mountains Silvretta Allgäu Alps Samnaun Mountains Mieming Mountains Western Tuxer Alps Eastern Tuxer Alps Western Lechtal Alps Kalkkögel Central Lechtal Alps Glockturm Range Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Western Karwendel Mountains low earlier moderate 2800 later low 2800 later gliding_snow 2600 NE S W NW SE SW N E earlier very_poor few 2 glide wet_snow 2800 W SE NE NW SW N E S later poor some 2 loose gliding_snow 2600 W SE NE NW SW N E S later very_poor some 2 glide The danger of wet and gliding avalanches will increase during the day. Small and medium-sized wet and gliding avalanches are possible as a consequence of warming during the day and solar radiation. This applies in particular on steep north and east facing slopes below approximately 2200 m, and elsewhere below approximately 2600 m. In addition the mostly small wind slabs adjacent to ridgelines on north facing slopes are capable of being triggered in very isolated cases still, in particular in high Alpine regions. Restraint should be exercised because avalanches can sweep people along and give rise to falls. The surface of the snowpack will freeze to form a strong crust and will soften during the day. The somewhat older wind slabs are lying on soft layers in particular on very steep shady slopes at elevated altitudes. Faceted weak layers exist deeper in the old snowpack on little used shady slopes. The snowpack will be generally subject to considerable local variations. Below the tree line only a little snow is now lying. The surface of the snowpack will cool hardly at all during the overcast night. Down to 1500 m snow will fall over a wide area. steady 2025-03-28T16:00:00Z 2025-03-29T16:00:00Z 2025-03-28 DP10 DP6