2026-04-04T15:00:00Z 2026-04-04T15:00:00Z 2026-04-05T15:00:00Z false Andreas Pecl Pre Alps Bregenzerwald Mountains moderate earlier considerable later wind_slab 1800 NW E NE N earlier slab wet_snow NW E SE S SW W NE N earlier loose wet_snow NW S SW SE W N NE E later loose Predominantly good backcountry touring conditions Slab avalanches can be triggered by large additional loading and grow to medium size. Danger zones occur in steep ridgeline terrain, behind sharp drops in the landscape, in wind-loaded gullies and bowls. In very steep terrain, wet-snow slides and avalanches are possible due to solar radiation and daytime warming. On steep grass-covered slopes, gliding snow activity is gradually increasing. steady 2026-04-05T15:00:00Z 2026-04-06T15:00:00Z 2026-04-05 2026-04-04T15:00:00Z 2026-04-04T15:00:00Z 2026-04-05T15:00:00Z false Andreas Pecl Rätikon East Rätikon West Silvretta West Lechquellen Mountains Allgäu Alps West Lechtal Alps Vorarlberg Verwall West moderate earlier considerable 2400 later moderate 2400 later persistent_weak_layers 2200 NW E W NE N earlier slab wet_snow 2200 E SE S SW W earlier loose wet_snow 2400 E SE S SW W later loose persistent_weak_layers 2200 NW E W NE N later slab Generally good backcountry touring conditions Slab avalanches can be triggered by large additional loading and grow to medium size. Danger zones occur in steep ridgeline terrain, behind sharp drops in the landscape, in wind-loaded gullies and bowls. Particularly in the northern half of high altitude zones, isolated avalanches can fracture in the weak layers in the uppermost metre of the snowpack. In very steep terrain, wet-snow slides and avalanches are possible due to solar radiation and daytime warming. On steep grass-covered slopes, gliding snow activity is gradually increasing. steady 2026-04-05T15:00:00Z 2026-04-06T15:00:00Z 2026-04-05