2025-01-19T16:00:00Z 2025-01-19T16:00:00Z 2025-01-20T16:00:00Z false Kauner Ridge Weißkugel Range Gurgler Range Western Verwall Mountains Central Stubai Alps Eastern Verwall Mountains Northern Zillertal Alps Silvretta Samnaun Mountains Mieming Mountains Western Tuxer Alps Eastern Tuxer Alps Glockturm Range Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Western Karwendel Mountains low 2200 all_day moderate 2200 all_day wind_slab 2200 NW NE N all_day poor some 1 slab Wind slabs require caution. As a consequence of a strong southerly foehn wind, mostly shallow wind slabs formed. These can still be released in some cases in particular on very steep shady slopes above approximately 2200 m. The avalanche prone locations are to be found in particular in gullies and bowls, and behind abrupt changes in the terrain. The wind slabs are clearly recognisable to the trained eye. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Avalanches can in very isolated cases penetrate near-ground layers of the snowpack and reach medium size. This applies in particular south of the Inn. As a consequence of a sometimes strong wind from southerly directions, mostly small wind slabs formed since Saturday, in particular in the regions exposed to the foehn wind. The wind slabs are in some cases still prone to triggering on steep shady slopes at elevated altitudes. Only a small amount of snow is lying for the time of year. The snowpack will be subject to considerable local variations. Shady slopes: The snowpack consists of faceted crystals. Isolated avalanche prone weak layers exist in the bottom section of the snowpack. Steep sunny slopes: As a consequence of mild temperatures and solar radiation a crust formed on the surface. The weather conditions will facilitate a gradual stabilisation of the snow drift accumulations. Further decrease in danger of dry avalanches. decreasing 2025-01-20T16:00:00Z 2025-01-21T16:00:00Z 2025-01-20 DP6 DP7 2025-01-19T16:00:00Z 2025-01-19T16:00:00Z 2025-01-20T16:00:00Z false Glockner Range Venediger Range Upper Passeier Valley Ratschings Durreck Range Langtaufers Upper Ahr Valley Southern Stubai Alps Southern Zillertal Alps Pfitsch Southern Sesvenna Group Ortler Range Schnals Ridge Northern Sesvenna Group Southern Adamello Adamello - Presanella Northern Brenta - Peller Southern Brenta Sole, Pejo and Rabbi Maddalene low 2200 all_day moderate 2200 all_day wind_slab 2200 NW NE N all_day poor some 1 slab Wind slabs require caution. The more recent wind slabs can still be released in some cases in particular on very steep shady slopes above approximately 2200 m, especially at transitions into gullies and bowls. The mostly small wind slabs are clearly recognisable to the trained eye. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Avalanches can in very isolated cases penetrate near-ground layers of the snowpack and reach medium size. Only a small amount of snow is lying for the time of year. Snow depths vary greatly, depending on the infuence of the wind. The more recent wind slabs are lying on unfavourable layers in particular on steep shady slopes at high altitudes and in high Alpine regions. Shady slopes: The snowpack consists of faceted crystals. Isolated avalanche prone weak layers exist in the old snowpack. Steep sunny slopes: As a consequence of mild temperatures and solar radiation a crust formed on the surface. The weather conditions will facilitate a gradual stabilisation of the snow drift accumulations. Further decrease in danger of dry avalanches. decreasing 2025-01-20T16:00:00Z 2025-01-21T16:00:00Z 2025-01-20 DP6 DP7 2025-01-19T16:00:00Z 2025-01-19T16:00:00Z 2025-01-20T16:00:00Z false Western Lechtal Alps Central Lechtal Alps Eastern Lechtal Alps Ammergau Alps Allgäu Alps low all_day The backcountry and freeriding conditions are mostly favourable. Wind slabs require caution. As a consequence of a moderate to strong wind from southerly directions, small wind slabs formed adjacent to ridgelines and in gullies and bowls. These can be released by a single winter sport participant in isolated cases in particular on extremely steep shady slopes above approximately 2200 m. The avalanche prone locations are rather rare and are clearly recognisable to the trained eye. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Wind slabs are lying on soft layers on shady slopes above approximately 2200 m. The old snowpack will be quite well bonded. Shady slopes: The snowpack consists of faceted crystals. Steep sunny slopes: As a consequence of mild temperatures and solar radiation a crust formed on the surface. The avalanche conditions are generally favourable. steady 2025-01-20T16:00:00Z 2025-01-21T16:00:00Z 2025-01-20 DP6 2025-01-19T16:00:00Z 2025-01-19T16:00:00Z 2025-01-20T16:00:00Z false Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Lasörling Range Gröden Dolomites Lüsner Mountains Sexten Dolomites Eastern Pfunderer Mountains Rieserferner Mountains Western Deferegger Alps Ulten Valley Eastern Nonsberger Alps Planeil Mountains Saldurn-Mastaun Ridge Northern Dolomites of Fiemme Hirzer Range Prags Dolomites Western Pfunderer Mountains Mount Saint Jakob Range Southern Sarntal Alps Texel Mountains Latemar Primiero - Pale di S. Martino Prealps Cembra Valley Bondone and Stivo Vallarsa Folgaria - Laverone Western Nonsberg Alps Fassa Valley Southern Lagorai Northern Lagorai Ledro Valley Paganella Pine' - Mocheni Valley Marzola - Valsugana low all_day Low avalanche danger will prevail. The old wind slabs are small and can only be released in isolated cases. Individual avalanche prone locations are to be found on extremely steep shady slopes at elevated altitudes, in particular in gullies and bowls. Such avalanche prone locations are rare and are easy to recognise. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Only a small amount of snow is lying for the time of year. The snowpack will be subject to considerable local variations. Shady slopes: The snowpack consists of faceted crystals. Steep sunny slopes: As a consequence of mild temperatures and solar radiation a crust formed on the surface. Low avalanche danger will prevail. steady 2025-01-20T16:00:00Z 2025-01-21T16:00:00Z 2025-01-20 DP6 2025-01-19T16:00:00Z 2025-01-19T16:00:00Z 2025-01-20T16:00:00Z false Brandenberg Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps Eastern Karwendel Mountains Central Kitzbühel Alps Western Kitzbühel Alps low all_day A mostly favourable avalanche situation will prevail. The small wind slabs can be released by a single winter sport participant in isolated cases in particular on extremely steep shady slopes at elevated altitudes. Caution is to be exercised on near-ridge slopes, as well as in gullies and bowls. The avalanche prone locations are rather rare and are clearly recognisable to the trained eye. Wind slabs are to be avoided in particular in terrain where there is a danger of falling. Wind slabs are lying on soft layers in particular on shady slopes at elevated altitudes. Shady slopes: The snowpack consists of faceted crystals. Steep sunny slopes: As a consequence of mild temperatures and solar radiation a crust formed on the surface. A favourable avalanche situation will be encountered over a wide area. steady 2025-01-20T16:00:00Z 2025-01-21T16:00:00Z 2025-01-20 DP6