Innsbruck sits deep in an Alpine valley in western Austria and receives around 900 mm (about 35 inches) of rain a year, with a strong summer peak as the surrounding high mountains trigger intense convective storms most afternoons during the warmer months. The narrow valley setting means that heavy rain can trigger fast-moving flash floods and debris flows from the steep slopes above the city, a well-recognized regional hazard during the wettest summer weeks. Winter brings heavy snow rather than rain at higher elevations nearby. Because the mountains create such localized, fast-changing weather, radar tracking is especially valuable here compared with flatter regions. GeoSphere Austria operates the national radar network.
Learn more: How Does Rain Radar Work? · Open the full Rain Map