2026-03-25T16:00:00Z2026-03-25T16:00:00Z2026-03-26T16:00:00ZfalseFlorian HerlaRätikon WestLechquellen MountainsLechtal Alps VorarlbergAllgäu Alps Westconsiderabletreelineall_dayhightreelineall_daynew_snowtreelineSEWESNENSWNWall_dayslabnew_snowtreelineSEWESNENSWNWall_dayslabpersistent_weak_layers2200WENENNWall_dayslabCaution: small snowdriftsAs a result of intensifying winds, small-sized freshly generated snowdrift accumulations can be triggered as small-to-medium sized slab avalanches. Danger zones occur primarily behind steep drops in the terrain and in wind-loaded gullies and bowls. Frequency and spread of avalanche prone locations increase with ascending altitude. Furthermore, avalanches can fracture in weak layers of the old snow from large additional loading and in isolated cases then grow to medium size. Such isolated avalanche prone locations occur in spots where the snow is shallow or in transitions from shallow to deep snow. As a result of strong solar radiation, small wet loose-snow avalanches can trigger in extremely steep terrain.decreasing2026-03-26T16:00:00Z2026-03-27T16:00:00Z2026-03-262026-03-25T16:00:00Z2026-03-25T16:00:00Z2026-03-26T16:00:00ZfalseFlorian HerlaBregenzerwald Mountainsconsiderableall_daynew_snowWNESEENSWNWSall_dayslabBeware small snowdriftsAvalanche danger is predominantly low. As winds intensify, however, fresh small-sized drifts can easily be triggered as small avalanches, particularly near ridgelines and behind sharp drops in the terrain. In addition, isolated avalanches can be triggered by large additional loading in extremely steep terrain. Apart from the risks of being buried in snow masses, the danger of being swept along and forced to take a fall require attentiveness.steady2026-03-26T16:00:00Z2026-03-27T16:00:00Z2026-03-262026-03-25T16:00:00Z2026-03-25T16:00:00Z2026-03-26T16:00:00ZfalseFlorian HerlaRätikon EastSilvretta WestVerwall Westconsiderableall_daynew_snowNEWSESWNWENSall_dayslabpersistent_weak_layers2200NEWNWENall_dayslabCaution: small snowdriftsAs a result of intensifying winds, small-sized freshly generated snowdrift accumulations can be triggered as small-to-medium sized slab avalanches. Danger zones occur primarily behind steep drops in the terrain and in wind-loaded gullies and bowls. Frequency and spread of avalanche prone locations increase with ascending altitude. Furthermore, avalanches can fracture in weak layers of the old snow from large additional loading and in isolated cases then grow to medium size. Such isolated avalanche prone locations occur in spots where the snow is shallow or in transitions from shallow to deep snow. As a result of strong solar radiation, small wet loose-snow avalanches can trigger in extremely steep terrain.steady2026-03-26T16:00:00Z2026-03-27T16:00:00Z2026-03-262026-03-25T16:00:00Z2026-03-25T16:00:00Z2026-03-26T16:00:00ZfalseFlorian HerlaPre Alpsmoderateall_daywind_slabWNENESESWNWSall_dayslabdecreasing2026-03-26T16:00:00Z2026-03-27T16:00:00Z2026-03-26