2024-01-01T16:00:00Z 2024-01-01T23:00:00Z 2024-01-02T23:00:00Z false Kauner Ridge Western Verwall Mountains Eastern Verwall Mountains Silvretta Samnaun Mountains Western Tuxer Alps Eastern Tuxer Alps Eastern Kitzbühel Alps Glockturm Range Eastern Karwendel Mountains Western Karwendel Mountains Eastern Lechtal Alps Ammergau Alps Weißkugel Range Central Kitzbühel Alps Western Kitzbühel Alps Gurgler Range Central Stubai Alps Northern Zillertal Alps Allgäu Alps Venediger Range Mieming Mountains Brandenberg Alps Wilder Kaiser Mountains - Waidring Alps Western Lechtal Alps Central Lechtal Alps Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Upper Passeier Valley Upper Ahr Valley Durreck Range Langtaufers Southern Zillertal Alps Southern Stubai Alps Pfitsch Schnals Ridge Northern Sesvenna Group moderate all_day wind_slab 2200 NE N E NW all_day poor few 2 gliding_snow 2600 SW S W E SE all_day very_poor few 2 Wind slabs and gliding snow require caution. As a consequence of the strong wind, fresh snow drift accumulations will form. These are prone to triggering at elevated altitudes. Caution is to be exercised in particular adjacent to ridgelines in gullies and bowls, and behind abrupt changes in the terrain above approximately 2200 m. The number and size of avalanche prone locations will increase with altitude. These avalanche prone locations are easy to recognise. In addition a moderate (level 2) danger of gliding avalanches exists, in particular on steep east, south and west facing slopes below approximately 2600 m. Gliding avalanches can be released at any time of day or night. Caution is to be exercised in areas with glide cracks. Over a wide area 5 to 20 cm of snow fell on Sunday above approximately 1000 m. In the Venediger Range up to 30 cm of snow fell on Sunday above approximately 1000 m. The wind will be moderate to strong in some regions. The fresh wind slabs are lying on soft layers at elevated altitudes. The fresh wind slabs can in some cases be released easily. The new snow is lying on a crust in all aspects below approximately 2600 m. Low and intermediate altitudes: The old snowpack is fairly homogeneous and its surface has a melt-freeze crust that is strong in many cases. This also applies on steep sunny slopes at high altitude. The old snowpack will be stable over a wide area. Fresh wind slabs require caution. A latent danger of gliding avalanches exists. steady 2024-01-02T23:00:00Z 2024-01-03T23:00:00Z 2024-01-02 DP6 DP2 2024-01-01T16:00:00Z 2024-01-01T23:00:00Z 2024-01-02T23:00:00Z false Glockner Range Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Lasörling Range Gröden Dolomites Lüsner Mountains Sexten Dolomites Eastern Pfunderer Mountains Ratschings Rieserferner Mountains Western Deferegger Alps Southern Sesvenna Group Ortler Range Ulten Valley Planeil Mountains Saldurn-Mastaun Ridge Hirzer Range Prags Dolomites Western Pfunderer Mountains Mount Saint Jakob Range Texel Mountains Southern Adamello Primiero - Pale di S. Martino Adamello - Presanella Northern Brenta - Peller Southern Brenta Fassa Valley Southern Lagorai Sole, Pejo and Rabbi Northern Lagorai Latemar Maddalene Pine' - Mocheni Valley low 2200 all_day moderate 2200 all_day wind_slab 2200 NE N E NW all_day poor few 2 Fresh wind slabs require caution. As a consequence of the strong wind, fresh snow drift accumulations will form. These are prone to triggering at elevated altitudes. Caution is to be exercised in particular adjacent to ridgelines in gullies and bowls, and behind abrupt changes in the terrain above approximately 2200 m. These avalanche prone locations are easy to recognise. In addition a certain danger of gliding avalanches exists. This applies in the regions with a lot of snow on steep east, south and west facing slopes below approximately 2600 m. Caution is to be exercised in areas with glide cracks. Over a wide area 10 to 20 cm of snow, and even more in some localities, fell on Sunday above approximately 1000 m. The wind will be moderate to strong in some regions. The fresh wind slabs are lying on soft layers at elevated altitudes. The fresh wind slabs can in some cases be released easily. Towards its base, the snowpack is faceted. The amount of snow is subject to significant local variations above the tree line. Low and intermediate altitudes: The old snowpack is fairly homogeneous and its surface has a melt-freeze crust that is strong in many cases, this also applies on steep sunny slopes at high altitude. Fresh wind slabs require caution. A certain danger of gliding avalanches exists. steady 2024-01-02T23:00:00Z 2024-01-03T23:00:00Z 2024-01-02 DP6 DP2