2026-03-02T16:00:00Z 2026-03-02T16:00:00Z 2026-03-03T16:00:00Z false Goldberg Group South Sadnig Group Schober Group East Ankogel-Hochalm Group Hafner Group Glockner Group Pasterze Kauner Ridge Zillertal Alps Northeast Zillertal Alps Northwest Grieskogel Mountains Goldried Glockner Group South Samnaun Mountains Tuxer Alps West Tuxer Alps East Glockturm Group Weißkugel Group Kitzbühel Alps Wildschönau Kitzbühel Alps Brixental Gurgler Group Stubai Alps Central Venediger Group South Lasörling Group Deferegger Alps East Schober Group West Kalkkögel Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Ratschings Stubai Alps South Upper Passeier Valley Texel Mountains Upper Ahr Valley Zillertal Alps South Pfitsch Sesvenna Group South Schnals Ridge Sesvenna Group North Saldurn-Mastaun Ridge Pfunderer Mountains West Pfunderer Mountains East Durreck Range Langtaufers Rieserferner Mountains Deferegger Alps West Ortler Range Ulten Valley Planeil Mountains Southern Adamello Adamello - Presanella Northern Brenta - Peller Southern Brenta Maddalene Sole, Pejo and Rabbi low 2000 all_day considerable 2000 all_day persistent_weak_layers 2000 E W N NW NE all_day poor some 3 slab Weakly bonded old snow represents the main danger. Avalanches can be released in the old snowpack and reach large size. This applies even in case of a single winter sport participant. The avalanche prone locations are to be found especially on west, north and east facing slopes above approximately 2000 m and in all aspects at elevated altitudes. Caution is to be exercised in particular at transitions from a shallow to a deep snowpack. Whumpfing sounds can indicate the danger. Remotely triggered avalanches are possible. In their paths avalanches can entrain the wet snow. This extends the avalanche runout distances. Outgoing longwave radiation during the night will be severely restricted. Individual small and, in isolated cases, medium-sized wet avalanches are possible below approximately 2200 m. Shady slopes: Distinct weak layers exist in the old snowpack in particular on west, north and east facing slopes. The surface of the snowpack will only just freeze. The weather conditions gave rise to thorough wetting of the snowpack below approximately 2200 m. Weakly bonded old snow requires caution. Single winter sport participants can release avalanches as before. Slight increase in danger of wet avalanches as a consequence of warming during the day and solar radiation. steady 2026-03-03T16:00:00Z 2026-03-04T16:00:00Z 2026-03-03 DP1 DP10 2026-03-02T16:00:00Z 2026-03-02T16:00:00Z 2026-03-03T16:00:00Z false Kreuzeck Group Carnic Alps Lesachtal Gailtal Alps West Carnic Alps Plöckenpass Reisseck Group Lienz Dolomites Kreuzeck Group East Tirol Carnic Alps East Tirol Gröden Dolomites Lüsner Mountains Sexten Dolomites Prags Dolomites Hirzer Range Mount Saint Jakob Range Latemar Primiero - Pale di S. Martino Vallarsa Folgaria - Lavarone Fassa Valley Southern Lagorai Northern Lagorai Marzola - Valsugana Pine' - Mocheni Valley low 2000 all_day moderate 2000 all_day persistent_weak_layers 2000 E W N NW NE all_day poor few 3 slab Weakly bonded old snow requires caution. Avalanches can in some cases be released in the old snowpack and reach quite a large size on west, north and east facing slopes. This applies even in case of a single winter sport participant in some cases. The avalanche prone locations are to be found in particular above approximately 2000 m. Caution is to be exercised in particular at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. Such avalanche prone locations are barely recognisable for beginners. In little used backcountry terrain the likelihood of avalanches is higher. Outgoing longwave radiation during the night will be reduced. Individual mostly small wet avalanches are possible below approximately 2200 m. Shady slopes: Distinct weak layers exist in the old snowpack in particular on west, north and east facing slopes. This applies especially above approximately 2000 m. The surface of the snowpack will only just freeze. The weather conditions gave rise to thorough wetting of the snowpack below approximately 2200 m. Weakly bonded old snow requires caution. Slight increase in danger of wet avalanches as a consequence of warming during the day and solar radiation. steady 2026-03-03T16:00:00Z 2026-03-04T16:00:00Z 2026-03-03 DP1 DP10 2026-03-02T16:00:00Z 2026-03-02T16:00:00Z 2026-03-03T16:00:00Z false Sarntal Alps South Nonsberger Alps East Dolomites of Fiemme North Prealps Cembra Valley Bondone and Stivo Western Nonsberg Alps Ledro Valley Paganella low treeline all_day moderate treeline all_day persistent_weak_layers treeline N NW NE all_day poor few 2 slab Weak layers in the old snowpack can still be released in isolated cases. Avalanches can in isolated cases be released in the old snowpack and reach medium size in isolated cases on northwest, north and northeast facing slopes. This applies in case of a single winter sport participant. In their paths avalanches can entrain the wet snow. As a consequence of warming during the day individual wet avalanches are possible. Distinct weak layers exist in the old snowpack in particular on west, north and east facing slopes. Outgoing longwave radiation during the night will be reduced. The weather conditions as the day progresses will give rise to thorough wetting of the snowpack. Weakly bonded old snow and wet snow require caution. steady 2026-03-03T16:00:00Z 2026-03-04T16:00:00Z 2026-03-03 DP1 DP10