2026-02-24T16:00:00Z 2026-02-24T16:00:00Z 2026-02-25T16:00:00Z false Glockner Group Pasterze Tuxer Alps West Tuxer Alps East Zillertal Alps Northeast Zillertal Alps Northwest Kitzbühel Alps Wildschönau Glockner Group South Kitzbühel Alps Brixental Venediger Group South Upper Ahr Valley considerable treeline all_day high treeline all_day persistent_weak_layers treeline E N W NE NW all_day poor many 3 slab wind_slab treeline E SE N W SW NE NW S all_day poor some 2 slab wet_snow 2200 SE W SW S all_day very_poor some 2 loose Even single freeriders can release avalanches easily. As a consequence of warming, the natural activity of wet avalanches will appreciably increase. As a consequence of new snow and warming a dangerous avalanche situation will persist. As a consequence of new snow and a strong to storm force northwesterly wind, further wind slabs formed in gullies and bowls and behind abrupt changes in the terrain. The new snow and wind slabs of the last few days are lying on top of a weakly bonded old snowpack. This applies on west, north and east facing slopes. The avalanche prone locations are numerous, especially in areas close to the tree line, as well as above the tree line. Winter sport participants can release avalanches easily, including large ones. Remotely triggered avalanches are possible. As a consequence of warming during the day and solar radiation loose snow avalanches are to be expected as the day progresses. This applies in particular on steep sunny slopes. In particular on steep, rather lightly snow-covered east and west facing slopes the wet avalanches can penetrate even deep layers and reach large size in isolated cases. In addition gliding avalanches are possible. This applies especially on cut and grassy slopes below approximately 2000 m. 15 to 30 cm of snow, and even more in some localities, fell on Tuesday. The wind was strong to storm force in some cases. The wind has transported the new snow significantly. Further wind slabs formed. On Wednesday it will be very mild. The snowpack will be prone to triggering over a wide area. The new snow and wind slabs are lying on top of a weakly bonded old snowpack. Distinct weak layers exist in the bottom section of the old snowpack. This applies in particular on west, north and east facing slopes in areas close to the tree line, and above the tree line. The rain gave rise to thorough wetting of the snowpack at low and intermediate altitudes. As a consequence of warming and solar radiation, the activity of wet avalanches will increase. steady 2026-02-25T16:00:00Z 2026-02-26T16:00:00Z 2026-02-25 DP1 DP10 2026-02-24T16:00:00Z 2026-02-24T16:00:00Z 2026-02-25T16:00:00Z false Gröden Dolomites Lüsner Mountains Sexten Dolomites Zillertal Alps South Pfitsch Schnals Ridge Sesvenna Group South Sesvenna Group North Saldurn-Mastaun Ridge Hirzer Range Pfunderer Mountains West Mount Saint Jakob Range Pfunderer Mountains East Ratschings Durreck Range Langtaufers Rieserferner Mountains Stubai Alps South Deferegger Alps West Ortler Range Ulten Valley Planeil Mountains Prags Dolomites Upper Passeier Valley Texel Mountains moderate 1800 all_day considerable 1800 all_day persistent_weak_layers 1800 E N W NE NW all_day very_poor some 3 slab wind_slab 2400 E N W NE NW all_day poor many 2 slab wet_snow E SE W SW S all_day very_poor some 2 slab Weakly bonded old snow requires caution. In particular, however, the danger of wet avalanches will increase. Avalanches can be released in the old snowpack and reach large size in isolated cases on west, north and east facing slopes. This applies in case of a single winter sport participant. The avalanche prone locations are to be found in particular above approximately 1800 m. In their paths avalanches can entrain the wet snow. This extends the avalanche runout distances. The fresh wind slabs are prone to triggering in particular on steep west, north and east facing slopes at elevated altitudes. As a consequence of warming during the day and solar radiation small and medium-sized wet avalanches are to be expected. This applies in particular on very steep sunny slopes, and at the base of rock walls. The runout zones are to be treated with caution. 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 good at times. The weather conditions as the day progresses will give rise to thorough wetting of the snowpack. This applies especially on very steep sunny slopes below approximately 2400 m. As a consequence of warming and solar radiation, the activity of wet avalanches will appreciably increase. steady 2026-02-25T16:00:00Z 2026-02-26T16:00:00Z 2026-02-25 DP1 DP10 2026-02-24T16:00:00Z 2026-02-24T16:00:00Z 2026-02-25T16:00:00Z false Sarntal Alps South Nonsberger Alps East Dolomites of Fiemme North low treeline all_day moderate treeline all_day persistent_weak_layers treeline E NW W N NE all_day poor some 2 slab wet_snow E NW SE W S SW N NE all_day very_poor few 1 slab Weak layers in the old snowpack can be released in isolated cases. Avalanches can in isolated cases be released in the old snowpack and reach medium size on west, north and east 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 and solar radiation individual small and medium-sized wet avalanches are to be expected. 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 quite good over a wide area. The weather conditions as the day progresses will give rise to thorough wetting of the snowpack. Wet snow requires caution. steady 2026-02-25T16:00:00Z 2026-02-26T16:00:00Z 2026-02-25 DP1 DP10