2024-02-17T16:00:00Z 2024-02-17T23:00:00Z 2024-02-18T23:00:00Z 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 Langtaufers Durreck Range Southern Stubai Alps Rieserferner Mountains Western Deferegger Alps Ortler Range Ulten Valley Planeil Mountains Prags Dolomites Upper Passeier Valley Texel Mountains moderate 2400 all_day low 2400 all_day wet_snow 2400 SW S W SE E all_day very_poor few 2 Wet and gliding avalanches are the main danger. As the penetration by moisture increases individual wet and gliding avalanches are possible. This applies especially in case of releases originating from extremely steep, sunny starting zones below approximately 2400 m that still retain some snow. In steep gullies in particular the wet avalanches can in very isolated cases reach areas without any snow cover. <br/> <br/> Wind slabs can be released in isolated cases in particular on extremely steep shady slopes. Avalanche prone locations are to be found in particular in gullies and bowls, and behind abrupt changes in the terrain, in particular at high altitudes and in high Alpine regions. Mostly avalanches are small. Restraint should be exercised because avalanches can sweep people along and give rise to falls. In very isolated cases dry avalanches can also be released in the old snowpack. Avalanche prone locations are to be found in particular in little used terrain above approximately 2400 m, especially on very steep shady slopes. Some rain has fallen in particular in the north. The high humditiy gave rise on Saturday to increasing and thorough wetting of the snowpack over a wide area below approximately 2400 m. A partly overcast night. The surface of the snowpack will only just freeze and will soften quickly, especially on very steep sunny slopes below approximately 2400 m. These weather conditions will give rise to increasing softening of the snowpack. <br/> <br/> The snowpack will be subject to considerable local variations at high altitude. Above approximately 2400 m: In near-surface layers, there are multiple melt-freeze crusts sandwiches with faceted layers in between. These layers can still be occasionally triggered, although the thickness of the slab is usually thin. Towards its base, the snowpack is stable. <br/> <br/> At low and intermediate altitudes only a little snow is lying. As a consequence of a moderate to strong northwesterly wind, sometimes avalanche prone wind slabs will form. Some snow will fall in particular in the northwest. steady 2024-02-18T23:00:00Z 2024-02-19T23:00:00Z 2024-02-18 DP2 DP10 2024-02-17T16:00:00Z 2024-02-17T23:00:00Z 2024-02-18T23:00:00Z false Southern Sarntal Alps Eastern Nonsberger Alps Northern Dolomites of Fiemme low all_day Currently there are favourable conditions generally. Wind slabs can be released in isolated cases in particular on extremely steep shady slopes. Avalanche prone locations are to be found in particular in gullies and bowls, and behind abrupt changes in the terrain, in particular at high altitude. Mostly avalanches are small. Restraint should be exercised because avalanches can sweep people along and give rise to falls. <br/> <br/> Individual wet loose snow slides are possible below approximately 2400 m. In near-surface layers, there are multiple melt-freeze crusts sandwiches with faceted layers in between. These layers can still be occasionally triggered, although the thickness of the slab is usually thin. Towards its base, the snowpack is stable. <br/> <br/> At low and intermediate altitudes only a little snow is lying. As a consequence of a moderate to strong northwesterly wind, sometimes avalanche prone wind slabs will form. steady 2024-02-18T23:00:00Z 2024-02-19T23:00:00Z 2024-02-18