2026-04-09T15:34:24Z 2026-04-07T15:00:00Z 2026-04-08T15:00:00Z true Zillertal Alps Northeast Zillertal Alps Northwest Lechtal Alps East Ammergau Alps South Kauner Ridge Weißkugel Group Verwall Mountains Central Gurgler Group Stubai Alps Central Verwall Mountains East Allgäu Alps East Silvretta East Samnaun Mountains Venediger Group South Mieming Mountains Lechtal Alps West Lechtal Alps Central Glockturm Group Karwendel Mountains East Glockner Group South low 2400 earlier moderate 2400 earlier considerable 2600 later moderate 2600 later 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 2600 m, also on very steep sunny slopes at elevated altitudes. In addition individual small and medium-sized gliding avalanches are possible. Avalanche prone locations for dry avalanches are to be found on very steep west, north and east facing slopes above approximately 2600 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 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 2600 m, as well as 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 2200 m, as well as on steep sunny slopes in high Alpine regions. Outgoing longwave radiation during the night will be good over a wide area. The avalanche danger will increase during the day. steady 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z 2026-04-08 DP10 DP1 2026-04-09T15:34:24Z 2026-04-07T15:00:00Z 2026-04-08T15:00:00Z true Tuxer Alps West Tuxer Alps East Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Karwendel Mountains West Kitzbühel Alps Wildschönau Kitzbühel Alps Brixental low 2400 earlier moderate 2400 earlier considerable 2600 later moderate 2600 later The danger of wet avalanches will already increase in the late morning. 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, also on very steep sunny slopes at elevated altitudes. Avalanche prone locations for dry avalanches are to be found on very steep west, north and east facing slopes above approximately 2600 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 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 2600 m, as well as 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 2200 m, as well as on steep sunny slopes in high Alpine regions. Outgoing longwave radiation during the night will be good over a wide area. The avalanche danger will increase during the day. steady 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z 2026-04-08 DP10 DP1 2026-04-09T15:34:24Z 2026-04-07T15:00:00Z 2026-04-08T15:00:00Z true Brandenberg Alps Kaiser Mountains - Waidring Alps Kitzbühel Alps Wildseeloder moderate earlier moderate later Increase in avalanche danger as a consequence of warming during the day and solar radiation. As a consequence of warming during the day and the solar radiation, the likelihood of moist and wet avalanches being released will increase. This applies in all aspects in particular below approximately 2400 m. Avalanches can in particular be released in near-surface layers and reach medium size. (--), caution is to be exercised, including on very steep shady slopes at elevated altitudes. These avalanche prone locations are rare and are difficult to recognise. 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 at low and intermediate altitudes, as well as on steep sunny slopes at elevated altitudes. Towards its base, the snowpack consists of faceted crystals, especially on shady slopes at elevated altitudes. Outgoing longwave radiation during the night will be good over a wide area. The avalanche danger will increase a little during the day. steady 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z 2026-04-08 DP10 DP4 2026-04-09T15:34:24Z 2026-04-07T15:00:00Z 2026-04-08T15:00:00Z true Deferegger Alps East Schober Group West Goldried Lienz Dolomites Kreuzeck Group East Tirol Carnic Alps East Tirol Lasörling Group Rieserferner Mountains Deferegger Alps West low earlier moderate 2400 later low 2400 later 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 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. 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. The avalanche danger will increase during the day. steady 2026-04-08T15:00:00Z 2026-04-09T15:00:00Z 2026-04-08 DP7 DP10