2026-03-24T16:00:00Z 2026-03-24T16:00:00Z 2026-03-25T16:00:00Z false Reisseck Group Ankogel-Hochalm Group Hafner Group Kreuzeck Group Goldberg Group South Carnic Alps Lesachtal Sadnig Group Glockner Group Pasterze Gailtal Alps West Schober Group East Carnic Alps Plöckenpass Kauner Ridge Verwall Mountains Central Verwall Mountains East Silvretta East Samnaun Mountains Tuxer Alps West Tuxer Alps East Glockturm Group Karwendel Mountains West Lienz Dolomites Kreuzeck Group East Tirol Carnic Alps East Tirol Zillertal Alps Northeast Zillertal Alps Northwest Lechtal Alps East Kitzbühel Alps Brixental Allgäu Alps East Venediger Group South Mieming Mountains Lasörling Group Deferegger Alps East Schober Group West Lechtal Alps West Lechtal Alps Central Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Goldried Glockner Group South Sexten Dolomites Ratschings Gröden Dolomites Lüsner Mountains Upper Ahr Valley Zillertal Alps South Pfitsch Sesvenna Group South Sesvenna Group North Hirzer Range Pfunderer Mountains West Mount Saint Jakob Range Pfunderer Mountains East Durreck Range Langtaufers Rieserferner Mountains Deferegger Alps West Planeil Mountains Prags Dolomites low 2200 all_day moderate 2200 all_day persistent_weak_layers 2200 NW N E W NE all_day poor few 2 slab Weakly bonded old snow requires caution. Single winter sport participants can release avalanches in some places. These can in some cases be triggered in near-surface layers. Caution is to be exercised in particular on very steep northwest, north and northeast facing slopes above approximately 2200 m, as well as on very steep west and east facing slopes above approximately 2500 m, in isolated cases also on very steep southeast, south and southwest facing slopes in high Alpine regions. Mostly avalanches are medium-sized. Avalanche prone locations are to be found in gullies and bowls, and behind abrupt changes in the terrain and adjacent to ridgelines. They are difficult to recognise. Isolated whumpfing sounds can indicate the danger. Additionally in isolated cases avalanches can be triggered in near-ground layers. The avalanche prone locations are to be found in particular on very steep west, north and east facing slopes above approximately 2200 m. Such avalanche prone locations are rare but are barely recognisable. Especially transitions from a shallow to a deep snowpack are unfavourable. As a consequence of warming during the day and the solar radiation, the likelihood of moist avalanches being released will increase a little on very steep sunny slopes. Somewhat older wind slabs are lying on the unfavourable surface of an old snowpack, especially on very steep northwest, north and northeast facing slopes above approximately 2200 m, also on very steep west and east facing slopes above approximately 2500 m, as well as on very steep southeast, south and southwest facing slopes in high Alpine regions. Towards its base, the snowpack is faceted and weak, especially on shady slopes above approximately 2200 m. Steep sunny slopes: Sunshine and high temperatures will give rise to moistening of the snowpack. Increase in avalanche danger as a consequence of new snow and wind. increasing 2026-03-25T16:00:00Z 2026-03-26T16:00:00Z 2026-03-25 DP6 DP7 2026-03-24T16:00:00Z 2026-03-24T16:00:00Z 2026-03-25T16:00:00Z false Karawanks Central Karawanks West Carnic Alps Nassfeld low 1900 all_day moderate 1900 all_day persistent_weak_layers 1900 NW N NE all_day poor few 2 slab Individual avalanche prone locations are to be found on northwest, north and northeast facing slopes at elevated altitudes. Single winter sport participants can release avalanches in isolated cases. These can be triggered in near-surface layers. Avalanche prone locations are to be found in particular adjacent to ridgelines and in pass areas at elevated altitudes. Additionally in very isolated cases avalanches can also penetrate near-ground layers of the snowpack and reach medium size. Caution is to be exercised in particular on very steep northwest, north and northeast facing slopes above approximately 1900 m. As a consequence of warming during the day and the solar radiation, the likelihood of moist avalanches being released will increase a little on very steep sunny slopes. The mostly shallow wind slabs are lying on the unfavourable surface of an old snowpack, especially on very steep northwest, north and northeast facing slopes above approximately 1900 m. Towards its base, the snowpack is faceted and weak, especially on shady slopes above approximately 1900 m. Steep sunny slopes: The weather conditions will give rise to moistening of the snowpack. Increase in avalanche danger as a consequence of new snow and wind. increasing 2026-03-25T16:00:00Z 2026-03-26T16:00:00Z 2026-03-25 DP7 DP1 2026-03-24T16:00:00Z 2026-03-24T16:00:00Z 2026-03-25T16:00:00Z false Koralpe West Karawanks East Packalpe Goldeck Group Gailtal Alps East Carnic Alps Oistnering Gailtal Alps Central Villach Alps Gurktal Alps South Saualpe South Gurktal Alps Central Nockberge Central Nockberge South Saualpe North low all_day persistent_weak_layers 1900 NW N NE all_day fair few 2 slab Low avalanche danger will prevail. Avalanches can be released in near-ground layers, in particular by large additional loads. This applies especially on very steep northwest, north and northeast facing slopes above approximately 1900 m. The avalanche prone locations are rare but are barely recognisable. In very isolated cases avalanches are medium-sized. As a consequence of warming during the day and the solar radiation, the likelihood of moist avalanches being released will increase a little. Weak layers exist in the bottom section of the snowpack on northwest, north and northeast facing slopes. This applies in particular above approximately 1900 m. Steep sunny slopes: The weather conditions will give rise to moistening of the snowpack. Increase in avalanche danger as a consequence of new snow and wind. increasing 2026-03-25T16:00:00Z 2026-03-26T16:00:00Z 2026-03-25 DP1