2026-04-08T15:00:00Z 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z false Glockner Group Pasterze Kauner Ridge Verwall Mountains Central Verwall Mountains East Silvretta East Samnaun Mountains Tuxer Alps West Tuxer Alps East Glockturm Group Karwendel Mountains West Zillertal Alps Northeast Zillertal Alps Northwest Lechtal Alps East Ammergau Alps South Weißkugel Group Kitzbühel Alps Wildschönau Kitzbühel Alps Brixental Gurgler Group Stubai Alps Central Allgäu Alps East Venediger Group South Mieming Mountains Lasörling Group Deferegger Alps East Lechtal Alps West Lechtal Alps Central Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Goldried Glockner Group South Upper Ahr Valley Zillertal Alps South Pfitsch Schnals Ridge Sesvenna Group South Sesvenna Group North Saldurn-Mastaun Ridge Ratschings Durreck Range Langtaufers Stubai Alps South Rieserferner Mountains Ortler Range Planeil Mountains Upper Passeier Valley low 2400 earlier moderate 2400 earlier considerable 2800 later moderate 2800 later persistent_weak_layers 2400 N NW W NE E earlier poor few 3 slab wet_snow 2400 N NW W NE E SE S SW earlier fair few 2 slab wet_snow 2800 N NW W NE E SE S SW later poor some 3 slab persistent_weak_layers 2400 N NW W NE E later poor few 3 slab The danger of wet avalanches will already increase in the late morning. Weak layers in the old snowpack can be released in some places by individual winter sport participants. In the late morning as a consequence of warming during the day and solar radiation there will be a rapid increase in the danger of moist and wet avalanches. Avalanches can penetrate deep layers and reach large size in isolated cases. This applies in all aspects in particular below approximately 2400 m, as well as on very steep west, south and east facing slopes at high altitude. Avalanche prone locations for dry avalanches are to be found on very steep shady slopes above approximately 2400 m. The avalanche prone locations are difficult to recognise. Whumpfing sounds and the formation of shooting cracks when stepping on the snowpack can indicate the danger. In steep terrain there is a danger of falling on the hard snow surface. Outgoing longwave radiation during the night will be quite good. The surface of the snowpack has frozen to form a strong crust only at high altitudes and will already soften in the late morning. The snowpack will become increasingly wet all the way through. This applies in all aspects below approximately 2400 m, as well as on steep sunny slopes at high altitude. Isolated avalanche prone weak layers exist in the top section of the old snowpack. Towards its base, the snowpack consists of faceted crystals. This applies in particular on west, north and east facing slopes at high altitude, as well as on steep sunny slopes in high Alpine regions. Outgoing longwave radiation during the night will be reduced. The avalanche danger will already be elevated in the early morning. This applies in particular below approximately 2400 m. steady 2026-04-09T15:00:00Z 2026-04-10T15:00:00Z 2026-04-09 DP10 DP1 2026-04-08T15:00:00Z 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z false Ankogel-Hochalm Group Goldberg Group South low 2400 earlier moderate 2400 earlier moderate later persistent_weak_layers 2400 N NW W NE E earlier poor few 2 slab persistent_weak_layers 2400 N NW W NE E later poor few 2 slab wet_snow 2400 N NW W NE E SE S SW later poor few 2 slab Increase in avalanche danger as a consequence of warming during the day and solar radiation. Weak layers in the old snowpack can be released in isolated cases. The avalanche conditions in the morning are mostly favourable. As a consequence of warming during the day and the solar radiation, the likelihood of wet avalanches being released will increase. This applies in all aspects below approximately 2400 m, and on south facing slopes at elevated altitudes. Avalanches are medium-sized and can be released by a single winter sport participant. In isolated cases dry avalanches can also be released in the old snowpack. Avalanche prone locations are to be found in particular on very steep west, north and east facing slopes above approximately 2400 m. These places are difficult to recognise. Avalanches can reach medium size. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Outgoing longwave radiation during the night will be good. The surface of the snowpack will freeze to form a strong crust and will already soften in the late morning. The snowpack will become increasingly wet all the way through. This applies in all aspects below approximately 2400 m, and on steep sunny slopes at elevated altitudes. Isolated avalanche prone weak layers exist in the top section of the old snowpack. Towards its base, the snowpack consists of faceted crystals. This applies in particular on west, north and east facing slopes above approximately 2400 m. Hardly any decrease in danger of moist and wet avalanches as the temperature drops. steady 2026-04-09T15:00:00Z 2026-04-10T15:00:00Z 2026-04-09 DP10 DP1 2026-04-08T15:00:00Z 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z false Reisseck Group Hafner Group Kreuzeck Group Sadnig Group Schober Group East Schober Group West Kreuzeck Group East Tirol low earlier moderate 2400 later low 2400 later persistent_weak_layers 2400 N NW W NE E earlier poor none 2 slab persistent_weak_layers 2400 N NW W NE E later poor none 2 slab wet_snow 2400 N NW W NE E SE S SW later poor few 2 slab Increase in avalanche danger as a consequence of warming during the day and solar radiation. Weak layers in the old snowpack can still be released in very isolated cases. The avalanche conditions in the morning are mostly favourable. As a consequence of warming during the day and the solar radiation, the likelihood of wet avalanches being released will increase. This applies in all aspects below approximately 2400 m, and on south facing slopes at elevated altitudes. Sometimes avalanches are medium-sized and can be released also by a single winter sport participant. In very isolated cases dry avalanches can also be released in the old snowpack. Avalanche prone locations are to be found in particular on very steep west, north and east facing slopes above approximately 2400 m. Avalanches can reach medium size. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Outgoing longwave radiation during the night will be good. The surface of the snowpack will freeze to form a strong crust and will already soften in the late morning. Sunshine and high temperatures will give rise to increasing and thorough wetting of the snowpack. The old wind slabs are lying on top of a weakly bonded old snowpack in particular on west, north and east facing slopes above approximately 2400 m. Hardly any decrease in danger of moist and wet avalanches as the temperature drops. steady 2026-04-09T15:00:00Z 2026-04-10T15:00:00Z 2026-04-09 DP10 DP1 2026-04-08T15:00:00Z 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z false Karawanks East Koralpe West Karawanks Central Packalpe Goldeck Group Carnic Alps Lesachtal Gailtal Alps East Karawanks West Carnic Alps Oistnering Gailtal Alps Central Gailtal Alps West Carnic Alps Nassfeld Carnic Alps Plöckenpass Villach Alps Gurktal Alps South Saualpe South Gurktal Alps Central Nockberge Central Nockberge South Saualpe North Lienz Dolomites Carnic Alps East Tirol low earlier low later wet_snow N NW W NE E SE S SW later poor few 1 slab As the day progresses the likelihood of wet avalanches being released will increase a little. The avalanche conditions in the morning are mostly favourable. As a consequence of warming during the day and the solar radiation, the likelihood of wet avalanches being released will increase. This applies in all aspects. Avalanches are rather small but can be released also by a single winter sport participant. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Outgoing longwave radiation during the night will be quite good at times. The surface of the snowpack will freeze to form a strong crust and will already soften in the late morning. Sunshine and high temperatures will give rise to increasing and thorough wetting of the snowpack. Hardly any increase in avalanche danger. steady 2026-04-09T15:00:00Z 2026-04-10T15:00:00Z 2026-04-09 DP10 DP1