2026-04-11T15:00:00Z 2026-04-11T15:00:00Z 2026-04-12T15:00:00Z 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 Weißkugel Group 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 Glockner Group South Upper Ahr Valley Zillertal Alps South Pfitsch Schnals Ridge Sesvenna Group South Sesvenna Group North Saldurn-Mastaun Ridge Durreck Range Langtaufers Rieserferner Mountains Stubai Alps South Ortler Range Planeil Mountains Upper Passeier Valley considerable 3000 all_day moderate 3000 all_day low all_day wet_snow 3000 SW NE S W NW E SE N all_day very_poor some 3 slab persistent_weak_layers 2400 NE W NW E N all_day poor few 3 slab The danger of moist and wet avalanches will already be elevated in the early morning. The danger of moist and wet avalanches will already be elevated in the early morning. As the day progresses as a consequence of warming during the day and solar radiation there will be an additional increase in the danger. This applies in all aspects below approximately 2400 m, as well as on very steep sunny slopes below approximately 3000 m. Avalanches can penetrate deep layers and reach large size. Individual avalanche prone locations for dry avalanches are to be found on very steep shady slopes above approximately 2400 m. Such avalanche prone locations are difficult to recognise. Especially transitions from a shallow to a deep snowpack are unfavourable. In addition the fresh wind slabs in high Alpine regions are prone to triggering in some cases, especially adjacent to ridgelines on very steep shady slopes. Wind slabs are mostly small. The surface of the snowpack will cool hardly at all during the overcast night. Sunshine and high temperatures will give rise as the day progresses to increasing and thorough wetting of the snowpack. This applies in all aspects below approximately 2400 m, as well as on 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 at high altitude, as well as in all aspects in high Alpine regions. As a consequence of mild temperatures and very cloudy skies the snowpack can not consolidate during the night. Up to high altitudes rain will fall on Monday in particular in the south. As a consequence of the rain, the likelihood of wet avalanches being released will increase in particular on steep shady slopes below approximately 2500 m. increasing 2026-04-12T15:00:00Z 2026-04-13T15:00:00Z 2026-04-12 DP10 DP1 2026-04-11T15:00:00Z 2026-04-11T15:00:00Z 2026-04-12T15:00:00Z false Carnic Alps Lesachtal Gailtal Alps West Carnic Alps Plöckenpass Lienz Dolomites Carnic Alps East Tirol low earlier moderate later wet_snow SW NE S W NW E SE N later poor some 1 loose Wet snow represents the main danger. 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 easily released. Avalanches can in isolated cases release deeper layers of the snowpack and reach medium size. Outgoing longwave radiation during the night will be reduced at times. The surface of the snowpack will freeze very little and will soften quickly. Sunshine and high temperatures gave rise to increasing and thorough wetting of the snowpack. Some rain will fall on Monday. As a consequence of the rain, the likelihood of wet avalanches being released will increase in particular on steep shady slopes below approximately 2500 m. increasing 2026-04-12T15:00:00Z 2026-04-13T15:00:00Z 2026-04-12 DP10 DP1 2026-04-11T15:00:00Z 2026-04-11T15:00:00Z 2026-04-12T15:00:00Z false Reisseck Group Kreuzeck Group Sadnig Group Schober Group East Schober Group West Goldried Kreuzeck Group East Tirol moderate all_day low all_day wet_snow SW NE S W NW E SE N all_day poor some 2 slab Wet snow represents the main danger. The danger of moist and wet avalanches will already exist in the early morning. This applies in all aspects below approximately 2400 m. As a consequence of warming during the day and the solar radiation, the likelihood of avalanches being released will increase especially on very steep sunny slopes below approximately 3000 m. Avalanches can in isolated cases penetrate near-ground layers of the snowpack and reach medium size. 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 shady slopes above approximately 2400 m. Outgoing longwave radiation during the night will be reduced at times. The surface of the snowpack will freeze very little and will soften quickly. The weather conditions will give rise to increasing and thorough wetting of the snowpack. Faceted weak layers exist in the bottom section of the old snowpack, especially on steep west, north and east facing slopes above approximately 2400 m. As a consequence of mild temperatures very cloudy skies the snowpack can not consolidate during the night. Some rain will fall on Monday. As a consequence of the rain, the likelihood of wet avalanches being released will increase in particular on steep shady slopes below approximately 2500 m. increasing 2026-04-12T15:00:00Z 2026-04-13T15:00:00Z 2026-04-12 DP10 DP1 2026-04-11T15:00:00Z 2026-04-11T15:00:00Z 2026-04-12T15:00:00Z false Brandenberg Alps Kaiser Mountains - Waidring Alps Kitzbühel Alps Wildseeloder Ammergau Alps South Karwendel Mountains East Kitzbühel Alps Wildschönau moderate all_day low all_day wet_snow SW NE S W NW E SE N all_day poor some 2 loose Wet snow represents the main danger. The danger of moist and wet avalanches will already be elevated in the early morning. As a consequence of warming during the day and the solar radiation, the likelihood of avalanches being released will increase a little. Wet avalanches can in very isolated cases penetrate near-ground layers of the snowpack and reach medium size, in particular on very steep shady slopes above approximately 2000 m. Outgoing longwave radiation during the night will be severely restricted. The surface of the snowpack will cool hardly at all during the overcast night. Sunshine and high temperatures will give rise as the day progresses to increasing and thorough wetting of the snowpack. Towards its base, the snowpack consists of faceted crystals, especially on shady slopes at elevated altitudes. Wet snow represents the main danger. steady 2026-04-12T15:00:00Z 2026-04-13T15:00:00Z 2026-04-12 DP10 DP1