2024-01-15T16:00:00Z 2024-01-15T23:00:00Z 2024-01-16T23:00:00Z false Western Lechtal Alps Central Lechtal Alps Eastern Lechtal Alps Allgäu Alps low treeline all_day considerable treeline all_day wind_slab treeline E SW S NW W N NE SE all_day poor many 2 Fresh wind slabs represent the main danger. The fresh wind slabs can be released by a single winter sport participant above the tree line. This also applies in areas close to the tree line. The wind slabs are clearly recognisable to the trained eye. They are to be avoided as far as possible. The avalanche prone locations are to be found in particular in gullies and bowls in all aspects. They are quite prevalent. Avalanches are medium-sized. Restraint should be exercised because avalanches can sweep people along and give rise to falls. In addition further very occasional gliding avalanches are possible, in particular on steep east, south and west facing slopes below approximately 2600 m. In isolated cases the gliding avalanches are quite large, in particular in the regions with a lot of snow. Areas with glide cracks are to be avoided. In some regions 10 to 15 cm of snow will fall. As a consequence of new snow and a sometimes strong wind from westerly directions, further wind slabs will form in the course of the day in particular in gullies and bowls and behind abrupt changes in the terrain. The fresh wind slabs are lying on surface hoar in some places. These are mostly rather small but prone to triggering. Towards its base, the snowpack is largely stable. Snow depths vary greatly above the tree line, depending on the infuence of the wind. The snowpack will be subject to considerable local variations. The fresh wind slabs remain for the foreseeable future prone to triggering. steady 2024-01-16T23:00:00Z 2024-01-17T23:00:00Z 2024-01-16 DP6 2024-01-15T16:00:00Z 2024-01-15T23:00:00Z 2024-01-16T23:00:00Z false Glockner Range Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Glockturm Range Weißkugel Range Gurgler Range Central Stubai Alps Northern Zillertal Alps Venediger Range Lasörling Range Gröden Dolomites Lüsner Mountains Sexten Dolomites Upper Ahr Valley Southern Zillertal Alps Pfitsch Southern Sesvenna Group Schnals Ridge Northern Sesvenna Group Saldurn-Mastaun Ridge Hirzer Range Western Pfunderer Mountains Mount Saint Jakob Range Eastern Pfunderer Mountains Ratschings Durreck Range Langtaufers Rieserferner Mountains Southern Stubai Alps Western Deferegger Alps Ortler Range Ulten Valley Planeil Mountains Northern Dolomites of Fiemme Prags Dolomites Upper Passeier Valley Texel Mountains low treeline all_day moderate treeline all_day wind_slab treeline E SW S NW W N NE SE all_day poor some 2 Fresh wind slabs are mostly easy to recognise and prone to triggering. The fresh wind slabs can be released easily in some cases above the tree line. This also applies in areas close to the tree line. The avalanche prone locations are to be found in particular adjacent to ridgelines and in gullies and bowls in all aspects. The wind slabs are clearly recognisable to the trained eye. They are to be avoided as far as possible. In isolated cases avalanches are medium-sized. Even a small avalanche can sweep winter sport participants along and give rise to falls. In addition further very occasional gliding avalanches are possible, in particular on steep east, south and west facing slopes below approximately 2600 m. In isolated cases the gliding avalanches are quite large, in particular in the regions with a lot of snow. Areas with glide cracks are to be avoided. As a consequence of a moderate to strong wind from westerly directions, further wind slabs will form in the course of the day. The fresh wind slabs are lying on surface hoar in some places. These are mostly rather small but can in some cases be released easily. Towards its base, the snowpack is largely stable. Snow depths vary greatly above the tree line, depending on the infuence of the wind. The snowpack will be subject to considerable local variations. In particular in the south 5 to 10 cm of snow, and even more in some localities, will fall. On Wednesday as a consequence of the strong southwesterly wind there will be an increase in the danger of dry avalanches. The fresh wind slabs remain prone to triggering. increasing 2024-01-16T23:00:00Z 2024-01-17T23:00:00Z 2024-01-16 DP6 2024-01-15T16:00:00Z 2024-01-15T23:00:00Z 2024-01-16T23:00:00Z false Ammergau Alps Kauner Ridge Central Kitzbühel Alps Western Verwall Mountains Western Kitzbühel Alps Eastern Verwall Mountains Silvretta Samnaun Mountains Mieming Mountains Western Tuxer Alps Eastern Tuxer Alps Brandenberg Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Eastern Karwendel Mountains Western Karwendel Mountains low treeline all_day moderate treeline all_day wind_slab treeline E SW S NW W N NE SE all_day poor some 2 Fresh wind slabs remain prone to triggering. The fresh wind slabs can be released by a single winter sport participant in some cases above the tree line. This also applies in areas close to the tree line. The avalanche prone locations are to be found in particular in gullies and bowls in all aspects. Avalanches are only shallow but easily released. They can reach medium size in isolated cases. The wind slabs are clearly recognisable to the trained eye. They are to be avoided as far as possible. Restraint should be exercised because avalanches can sweep people along and give rise to falls. In addition further very occasional gliding avalanches are possible, in particular on steep east, south and west facing slopes below approximately 2600 m. In isolated cases the gliding avalanches are quite large, in particular in the regions with a lot of snow. Areas with glide cracks are to be avoided. In some regions 5 to 10 cm of snow fell on Monday. As a consequence of a sometimes strong wind from westerly directions, further wind slabs will form in particular in gullies and bowls and behind abrupt changes in the terrain. The fresh wind slabs are lying on surface hoar in some places. These are mostly rather small but prone to triggering. Towards its base, the snowpack is largely stable. Snow depths vary greatly above the tree line, depending on the infuence of the wind. The snowpack will be subject to considerable local variations. The fresh wind slabs remain for the foreseeable future prone to triggering. steady 2024-01-16T23:00:00Z 2024-01-17T23:00:00Z 2024-01-16 DP6