2025-04-04T15:00:00Z 2025-04-04T15:00:00Z 2025-04-05T15:00:00Z false Kauner Ridge Weißkugel Range Western Verwall Mountains Gurgler Range Eastern Verwall Mountains Central Stubai Alps Silvretta Northern Zillertal Alps Samnaun Mountains Venediger Range Lasörling Range Western Tuxer Alps Glockner Range Eastern Tuxer Alps Eastern Deferegger Alps Schober Mountains Lienzer Dolomites Glockturm Range 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 low 2400 earlier moderate 2400 earlier moderate later persistent_weak_layers 2400 NW N E NE W earlier poor few 2 slab wet_snow 2800 SE S E W SW later poor few 3 slab persistent_weak_layers 2400 NW E W N NE later poor few 2 slab Increase in danger of wet avalanches as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution. As a consequence of warming during the day and solar radiation more frequent wet avalanches are possible. They can in some cases release the saturated snowpack and reach large size in isolated cases. This applies in particular on very steep sunny slopes below approximately 2800 m. Late morning: Weak layers in the old snowpack can be released in isolated cases by individual winter sport participants. These avalanche prone locations are to be found in particular on very steep shady slopes above approximately 2400 m and on very steep west and east facing slopes above approximately 2600 m. Afternoon: As a consequence of warming during the day and the solar radiation, the likelihood of slab avalanches being released will increase a little. Mostly the avalanches are medium-sized. Gliding avalanches can also occur. Caution is to be exercised on grassy slopes below approximately 2600 m. Outgoing longwave radiation during the night was good. The surface of the snowpack will freeze to form a strong crust. In steep terrain there is a danger of falling on the hard snow surface. The surface of the snowpack will soften during the day. Sunshine and high temperatures will give rise to increasing and thorough wetting of the snowpack in particular on sunny slopes below approximately 2800 m. Avalanche prone weak layers exist in the old snowpack especially on little used west, north and east facing slopes. This applies on shady slopes above approximately 2400 m, as well as on west and east facing slopes above approximately 2600 m. Decrease in danger of wet avalanches as the temperature drops. decreasing 2025-04-05T15:00:00Z 2025-04-06T15:00:00Z 2025-04-05 DP10 DP1 2025-04-04T15:00:00Z 2025-04-04T15:00:00Z 2025-04-05T15:00:00Z false Primiero - Pale di S. Martino Southern Adamello Adamello - Presanella Northern Brenta - Peller Fassa Valley Southern Brenta Southern Lagorai Sole, Pejo and Rabbi Northern Lagorai Latemar Maddalene low 2400 earlier moderate 2400 earlier low treeline later moderate treeline later persistent_weak_layers 2400 NW N NE earlier poor few 2 slab wet_snow treeline 2200 SE S E W SW earlier poor few 1 loose wet_snow treeline 2800 SE S E W SW later poor some 2 slab persistent_weak_layers 2400 NW N NE later poor few 2 slab Increase in danger of wet avalanches as a consequence of warming during the day and solar radiation. Weakly bonded old snow requires caution. During the day: As a consequence of warming during the day and the solar radiation, the likelihood of moist slab avalanches being released will increase significantly. Caution is to be exercised in particular on very steep sunny slopes below approximately 2800 m, as well as on very steep west facing slopes below approximately 2600 m. Avalanches can in some cases release the wet snowpack. Mostly the avalanches are medium-sized. Gliding avalanches can also occur, in particular on grassy slopes below approximately 2400 m. Early morning: Weak layers in the old snowpack can be released in isolated cases by individual winter sport participants. These avalanche prone locations are to be found in particular on very steep shady slopes above approximately 2400 m and on very steep west and east facing slopes above approximately 2600 m. As a consequence of warming during the day and the solar radiation, the likelihood of slab avalanches being released will increase appreciably. The surface of the snowpack has frozen to form a strong crust and will soften earlier than the day before. Sunshine and high temperatures will give rise to increasing and thorough wetting of the snowpack over a wide area in all aspects below approximately 2800 m. Avalanche prone weak layers exist in the old snowpack especially on little used west, north and east facing slopes. This applies on shady slopes above approximately 2400 m. The snowpack will be subject to considerable local variations at intermediate altitudes. Below the tree line a little snow is lying. Decrease in danger of wet avalanches as the temperature drops. steady 2025-04-05T15:00:00Z 2025-04-06T15:00:00Z 2025-04-05 DP10 DP2 2025-04-04T15:00:00Z 2025-04-04T15:00:00Z 2025-04-05T15:00:00Z false Eastern Lechtal Alps Ammergau Alps Central Kitzbühel Alps Western Kitzbühel Alps Allgäu Alps Mieming Mountains Brandenberg Alps Wilder Kaiser Mountains - Waidring Alps Western Lechtal Alps Eastern Kitzbühel Alps Central Lechtal Alps Eastern Karwendel Mountains Western Karwendel Mountains low earlier moderate later wet_snow SE E W S SW later poor few 2 loose Increase in danger of wet avalanches as a consequence of warming during the day and solar radiation. The backcountry touring conditions in the morning, after a clear night, are favourable. As a consequence of warming during the day and the solar radiation, the likelihood of wet avalanches being released will increase. Caution is to be exercised in particular on very steep sunny slopes. Avalanches can in some cases release the saturated snowpack. Gliding avalanches can also occur. This applies on grassy slopes below approximately 2600 m. Outgoing longwave radiation during the night was good. The surface of the snowpack will freeze to form a strong crust. In steep terrain there is a danger of falling on the hard snow surface. The surface of the snowpack will soften during the day. Sunshine and high temperatures will give rise to increasing and thorough wetting of the snowpack in particular on sunny slopes. Decrease in danger of wet avalanches as the temperature drops. decreasing 2025-04-05T15:00:00Z 2025-04-06T15:00:00Z 2025-04-05 DP10 DP2 2025-04-04T15:00:00Z 2025-04-04T15:00:00Z 2025-04-05T15:00:00Z false Prealps Cembra Valley Bondone and Stivo Vallarsa Western Nonsberg Alps Folgaria - Laverone Ledro Valley Paganella Pine' - Mocheni Valley Marzola - Valsugana low all_day The danger of moist and wet avalanches will increase during the day. Small and medium-sized wet and gliding avalanches are possible as a consequence of warming during the day and solar radiation. As a consequence of warming during the day and the solar radiation, the likelihood of wet slab avalanches being released will increase in particular on grassy slopes at low and intermediate altitudes. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Weak layers in the old snowpack can be released in some places in particular on steep shady slopes. These avalanche prone locations are rather rare and are difficult to recognise. The avalanche prone locations are to be found in particular on steep, little used shady slopes above approximately 1900 m. In isolated cases avalanches can also release deeper layers of the snowpack and reach medium size. Outgoing longwave radiation during the night was good. The surface of the snowpack has frozen to form a strong crust will soften earlier than the day before. Individual weak layers exist in the old snowpack especially on steep shady slopes. The snowpack will be generally subject to considerable local variations. Below the tree line a little snow is lying. Outgoing longwave radiation during the night was good. The surface of the snowpack has frozen to form a strong crust will soften earlier than the day before. Individual weak layers exist in the old snowpack especially on steep shady slopes. The snowpack will be generally subject to considerable local variations. Below the tree line a little snow is lying. Decrease in danger of wet avalanches as the temperature drops. steady 2025-04-05T15:00:00Z 2025-04-06T15:00:00Z 2025-04-05 DP10 DP2 2025-04-04T15:00:00Z 2025-04-04T15:00:00Z 2025-04-05T15:00:00Z false Southern Sarntal Alps Eastern Nonsberger Alps Northern Dolomites of Fiemme low all_day wet_snow 2800 SE E W S SW all_day very_poor few 1 slab The danger of moist and wet avalanches will increase during the day. Avalanches can in very isolated cases be released by a single winter sport participant. The avalanche prone locations are to be found in particular on very steep shady slopes at elevated altitudes. As a consequence of solar radiation individual wet avalanches are possible. This applies on steep sunny slopes, as well as on steep west facing slopes. In regions neighbouring those that are subject to danger level 3 (considerable) the avalanche prone locations are more prevalent and the danger is greater. Mostly avalanches are small. The surface of the snowpack will only just freeze and will soften quickly. Isolated avalanche prone weak layers exist in the old snowpack especially on steep shady slopes. The snowpack will be generally subject to considerable local variations. Only a little snow is now lying. Low avalanche danger will prevail. steady 2025-04-05T15:00:00Z 2025-04-06T15:00:00Z 2025-04-05