2024-01-11T16:00:00Z 2024-01-11T23:00:00Z 2024-01-12T23:00:00Z 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 Allgäu Alps Northern Zillertal Alps Venediger Range Mieming Mountains Lasörling Range Glockner Range Brandenberg Alps Eastern Deferegger Alps Wilder Kaiser Mountains - Waidring Alps Schober Mountains Western Lechtal Alps Lienzer Dolomites Central Lechtal Alps Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains 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 Southern Stubai Alps Rieserferner Mountains Western Deferegger Alps Ortler Range Ulten Valley Planeil Mountains Prags Dolomites Upper Passeier Valley Texel Mountains Latemar Southern Adamello Primiero - Pale di S. Martino Adamello - Presanella Northern Brenta - Peller Vallarsa Folgaria - Laverone Southern Brenta Fassa Valley Southern Lagorai Sole, Pejo and Rabbi Northern Lagorai Maddalene Paganella Pine' - Mocheni Valley Marzola - Valsugana 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 and older wind slabs require caution. The fresh and somewhat older wind slabs can be released by a single winter sport participant above the tree line. Caution is to be exercised in all aspects in gullies and bowls, and behind abrupt changes in the terrain. The number and size of avalanche prone locations will increase with altitude. <br/> <br/> In addition a latent danger of gliding avalanches exists, in particular on steep east, south and west facing slopes below approximately 2600 m. In isolated cases the gliding avalanches are quite large. As a consequence of a gathering strong wind from northerly directions, further wind slabs will form in the course of the day. The somewhat older wind slabs are lying on soft layers. The fresh wind slabs are lying on surface hoar in some places. <br/> <br/> 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 and older wind slabs remain in some cases prone to triggering. steady 2024-01-12T23:00:00Z 2024-01-13T23:00:00Z 2024-01-12 DP6 DP2