2026-03-05T16:00:00Z 2026-03-05T16:00:00Z 2026-03-06T16:00:00Z false Zillertal Alps Northeast Zillertal Alps Northwest Kauner Ridge Weißkugel Group Kitzbühel Alps Wildschönau Kitzbühel Alps Brixental Gurgler Group Stubai Alps Central Samnaun Mountains Tuxer Alps West Tuxer Alps East Glockturm Group Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Langtaufers Sesvenna Group South Ortler Range Sesvenna Group North Planeil Mountains 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 on west, north and east facing slopes above approximately 2000 m. As a consequence of warming during the day and the solar radiation, the likelihood of slab avalanches being released will increase a little also on steep sunny slopes 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 isolated cases. As a consequence of warming during the day and solar radiation only isolated mostly small wet avalanches are possible. Distinct weak layers exist in the old snowpack in particular on west, north and east facing slopes. This applies especially above approximately 2000 m. Towards its surface, the snowpack consists of faceted crystals, especially on shady slopes. Outgoing longwave radiation during the night will be quite good. The surface of the snowpack will freeze to form a strong crust. The weather conditions as the day progresses will give rise to slight softening of the snowpack in particular on very steep sunny slopes. 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 2026-03-06T16:00:00Z 2026-03-07T16:00:00Z 2026-03-06 DP7 DP10 2026-03-05T16:00:00Z 2026-03-05T16:00:00Z 2026-03-06T16:00:00Z false Carnic Alps Lesachtal Gailtal Alps West Kreuzeck Group Goldberg Group South Sadnig Group Carnic Alps Plöckenpass Schober Group East Reisseck Group Ankogel-Hochalm Group Hafner Group Glockner Group Pasterze Lienz Dolomites Kreuzeck Group East Tirol Carnic Alps East Tirol Venediger Group South Lasörling Group Deferegger Alps East Schober Group West Goldried Glockner Group South Gröden Dolomites Lüsner Mountains Sexten Dolomites Upper Ahr Valley Zillertal Alps South Pfitsch Schnals Ridge Saldurn-Mastaun Ridge Hirzer Range Pfunderer Mountains West Mount Saint Jakob Range Pfunderer Mountains East Durreck Range Ratschings Rieserferner Mountains Stubai Alps South Deferegger Alps West Ulten Valley Prags Dolomites Upper Passeier Valley Texel Mountains 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 large size in isolated cases 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. As a consequence of warming during the day and the solar radiation, the likelihood of slab avalanches being released will increase a little also on steep sunny slopes at elevated altitudes. Only isolated mostly small wet loose snow avalanches are possible. Distinct weak layers exist in the old snowpack in particular on west, north and east facing slopes. This applies especially above approximately 2000 m. Towards its surface, the snowpack consists of faceted crystals, especially on shady slopes. Outgoing longwave radiation during the night will be quite good. The surface of the snowpack will freeze to form a strong crust. The weather conditions as the day progresses will give rise to slight softening of the snowpack in particular on very steep sunny slopes. 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 2026-03-06T16:00:00Z 2026-03-07T16:00:00Z 2026-03-06 DP7 DP10 2026-03-05T16:00:00Z 2026-03-05T16:00:00Z 2026-03-06T16:00:00Z false Sarntal Alps South Nonsberger Alps East Dolomites of Fiemme North Prealps Cembra Valley Bondone and Stivo Western Nonsberg Alps Ledro Valley Paganella low all_day persistent_weak_layers treeline N NW NE all_day poor none 2 slab Weak layers in the old snowpack can still be released in isolated cases. Avalanches can in very 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. As a consequence of warming during the day individual wet avalanches are possible. Shady slopes: Avalanche prone weak layers exist in the old snowpack in particular on northwest, north and northeast facing slopes. Sunny slopes: The weather conditions gave rise to moistening of the snowpack below approximately 2500 m. The weather will be mild. Slight increase in danger of wet avalanches as a consequence of warming during the day and solar radiation. steady 2026-03-06T16:00:00Z 2026-03-07T16:00:00Z 2026-03-06 DP1 DP10