2025-02-03T16:00:00Z 2025-02-03T16:00:00Z 2025-02-04T16:00:00Z false Glockner Range Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Glockturm Range Weißkugel Range Gurgler Range Central Stubai 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 Prags Dolomites Upper Passeier Valley Texel Mountains low treeline all_day moderate treeline all_day persistent_weak_layers treeline W NE NW E N all_day poor few 3 slab Weakly bonded old snow requires caution. Weak layers in the old snowpack can be released in isolated cases by winter sport participants in particular in little used terrain. Avalanches can in some cases penetrate deep layers and reach large size. The avalanche prone locations are barely recognisable, even to the trained eye. <br/> Avalanche prone locations for dry avalanches are to be found in particular on steep west, north and east facing slopes above the tree line, in isolated cases also on steep shady slopes in areas close to the tree line. <br/> <br/> As a consequence of warming during the day and solar radiation individual wet loose snow slides are possible as the day progresses, especially on very steep sunny slopes. Above the tree line snow depths vary greatly, depending on the infuence of the wind. The snowpack will be subject to considerable local variations at elevated altitudes. <br/> The barely recognisable wind slabs are lying on top of a weakly bonded old snowpack in particular on west to north to east facing aspects above the tree line. This also applies in isolated cases on south facing slopes in high Alpine regions. The weather conditions will foster a stabilisation of the snowpack. <br/> <br/> Steep sunny slopes below approximately 2600 m: As a consequence of mild temperatures and solar radiation a crust will form on the surface during the night. Low and intermediate altitudes: The old snowpack is moist and its surface consists of loosely bonded snow lying on a crust that is strong in many cases. This applies in particular on shady slopes. Weakly bonded old snow requires caution. steady 2025-02-04T16:00:00Z 2025-02-05T16:00:00Z 2025-02-04 DP1 2025-02-03T16:00:00Z 2025-02-03T16:00:00Z 2025-02-04T16:00:00Z false Southern Sarntal Alps Eastern Nonsberger Alps Northern Dolomites of Fiemme low all_day Old wind slabs require caution. The avalanches can in isolated cases be released by large loads, caution is to be exercised in particular in gullies and bowls, and behind abrupt changes in the terrain. Avalanche prone locations for dry avalanches are to be found in particular on steep west, north and east facing slopes above the tree line. Mostly avalanches are small. <br/> <br/> As a consequence of warming during the day and solar radiation individual wet loose snow slides are possible as the day progresses, especially on very steep sunny slopes. The somewhat older wind slabs are in individual cases still prone to triggering in particular on shady slopes above the tree line. This applies in particular at high altitude. <br/> The old snowpack is moist and its surface consists of loosely bonded snow lying on a crust that is strong in many cases. This applies especially at low and intermediate altitudes. Wind slabs require caution. steady 2025-02-04T16:00:00Z 2025-02-05T16:00:00Z 2025-02-04 DP6