2023-12-16T16:00:00Z 2023-12-16T23:00:00Z 2023-12-17T23:00:00Z Glockner Range Glockturm Range Weißkugel Range Gurgler Range Central Stubai Alps Northern Zillertal Alps Venediger Range Durreck Range Langtaufers Upper Ahr Valley Southern Stubai Alps Southern Zillertal Alps Pfitsch Southern Sesvenna Group Ortler Range Schnals Ridge Northern Sesvenna Group Planeil Mountains Saldurn-Mastaun Ridge Upper Passeier Valley moderate 2200 all_day considerable 2200 all_day wind_slab 2200 SE E N S SW W NW NE all_day poor some 2 gliding_snow 2400 SE E S SW W all_day very_poor few 2 persistent_weak_layers 2200 E N W NW NE all_day fair few 3 Fresh wind slabs represent the main danger. Gliding snow requires caution. The fresh wind slabs remain in some cases prone to triggering. This applies in particular on shady slopes, also on sunny slopes at elevated altitudes. Caution is to be exercised in particular above approximately 2200 m, as well as in gullies and bowls, and behind abrupt changes in the terrain. Avalanches can be released easily and reach medium size. The prevalence of avalanche prone locations and likelihood of triggering will increase with altitude. Shooting cracks when stepping on the snowpack can indicate the danger. As a consequence of warming loose snow avalanches are to be expected, but they will be mostly small. In addition there is a danger of gliding avalanches. This applies on steep slopes below approximately 2400 m. Weak layers in the old snowpack can be released especially by large additional loads in particular at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. Individual avalanche prone locations are to be found on very steep shady slopes above approximately 2200 m. Avalanches can reach large size in isolated cases. The wind was strong in some cases. As a consequence of new snow and wind from northerly directions, sometimes large wind slabs formed. More recent wind slabs are lying on soft layers in all aspects at high altitudes and in high Alpine regions. Faceted weak layers exist in the centre of the snowpack in particular above approximately 2200 m. The weather conditions will foster a gradual settling of the snow drift accumulations. As a consequence of warming, the likelihood of wet loose snow avalanches being released will increase for a while in particular on very steep sunny slopes. decreasing 2023-12-17 DP6 DP2 2023-12-16T16:00:00Z 2023-12-16T23:00:00Z 2023-12-17T23:00:00Z Eastern Lechtal Alps Ammergau Alps Kauner Ridge Western Verwall Mountains Eastern Verwall Mountains Allgäu Alps Silvretta Samnaun Mountains Mieming Mountains Western Tuxer Alps Eastern Tuxer Alps Western Lechtal Alps Central Lechtal Alps Kalkkögel Grieskogel Mountains Serles Ridge Kühtai - Geigen Ridge Sellrain - Alpein Mountains Western Karwendel Mountains moderate all_day wind_slab 2200 SE E N S SW W NW NE all_day poor some 2 gliding_snow 2400 SE E S SW W all_day very_poor few 2 Fresh wind slabs represent the main danger. Gliding snow requires caution. The fresh wind slabs remain in some cases prone to triggering. This applies in particular on shady slopes, also on sunny slopes at elevated altitudes. Caution is to be exercised in particular above approximately 2200 m, as well as in gullies and bowls, and behind abrupt changes in the terrain. Avalanches can be released by a single winter sport participant and reach medium size. The prevalence of avalanche prone locations and likelihood of triggering will increase with altitude. Shooting cracks when stepping on the snowpack can indicate the danger. As a consequence of warming loose snow avalanches are to be expected, but they will be mostly small. In addition there is a danger of gliding avalanches. This applies on steep slopes below approximately 2400 m. Weak layers in the old snowpack can be released especially by large additional loads in particular at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. This applies in particular on very steep shady slopes above approximately 2200 m. These avalanche prone locations are very rare. Avalanches can reach large size in isolated cases. The wind was strong in some cases. As a consequence of new snow and wind from northerly directions, sometimes large wind slabs formed. More recent wind slabs are lying on soft layers in all aspects at high altitudes and in high Alpine regions. Faceted weak layers exist in the centre of the snowpack in particular above approximately 2200 m. As a consequence of rising temperatures the snowpack will settle during the next few days. As a consequence of warming, the likelihood of wet loose snow avalanches being released will increase for a while in particular on very steep sunny slopes. steady 2023-12-17 DP6 DP2 2023-12-16T16:00:00Z 2023-12-16T23:00:00Z 2023-12-17T23:00:00Z Brandenberg Alps Wilder Kaiser Mountains - Waidring Alps Eastern Kitzbühel Alps Eastern Karwendel Mountains Central Kitzbühel Alps Western Kitzbühel Alps moderate all_day gliding_snow SE E N S SW W NW NE all_day very_poor some 2 wind_slab treeline SE E N S SW W NW NE all_day poor some 2 Gliding snow represents the main danger. Fresh wind slabs require caution. As a consequence of warming more medium-sized gliding avalanches are possible. This applies on steep grassy slopes. The fresh wind slabs are in some cases prone to triggering on steep shady slopes. Caution is to be exercised in particular above the tree line, as well as in gullies and bowls, and behind abrupt changes in the terrain. The avalanche prone locations are covered with new snow and are therefore difficult to recognise. More recent wind slabs are lying on soft layers in particular on near-ridge shady slopes at elevated altitudes. As a consequence of rising temperatures the snow drift accumulations will stabilise. The old snowpack is wet, in particular at low and intermediate altitudes. Gradual increase in danger of gliding avalanches as a consequence of warming. increasing 2023-12-17 DP2 DP6 2023-12-16T16:00:00Z 2023-12-16T23:00:00Z 2023-12-17T23:00:00Z Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Lasörling Range Gröden Dolomites Lüsner Mountains Sexten Dolomites Eastern Pfunderer Mountains Ratschings Rieserferner Mountains Western Deferegger Alps Ulten Valley Prags Dolomites Hirzer Range Western Pfunderer Mountains Mount Saint Jakob Range Texel Mountains low 2200 all_day moderate 2200 all_day wind_slab 2200 E N W NW NE all_day poor some 2 Wind slabs require caution. The fresh and older wind slabs are in some cases prone to triggering above approximately 2200 m. The avalanche prone locations are to be found in particular in west to north to east facing aspects. Avalanches can be released by a single winter sport participant and reach medium size. Caution is to be exercised in particular adjacent to ridgelines and in gullies and bowls. As a consequence of warming loose snow avalanches are to be expected, but they will be mostly small. Weak layers in the old snowpack can be released in very isolated cases in particular at transitions from a shallow to a deep snowpack, when entering gullies and bowls for example. This applies on very steep shady slopes above approximately 2400 m, especially in the north. The avalanche prone locations are rare. Avalanches can reach medium size. As a consequence of a strong to storm force northwesterly wind, wind slabs formed in the last few days in gullies and bowls and behind abrupt changes in the terrain. These are lying on soft layers in particular on shady slopes at elevated altitudes. Faceted weak layers exist in the centre of the snowpack in particular above approximately 2400 m. Sunshine and high temperatures will give rise as the day progresses to slight moistening of the snowpack in particular on sunny slopes. The weather conditions will foster a gradual settling of the snow drift accumulations. As a consequence of warming, the likelihood of wet loose snow avalanches being released will increase further in particular on very steep sunny slopes. steady 2023-12-17 DP6 DP7