Veri: ICON, DWD (resolution 13 km)
Güncelleme: 12:00 UTC (bir sonraki güncelleme: 18:00 UTC - hazırlık)
Şu anki saat: 21:00, 10.04.2025 (UTC)

For this output data, temperature is shown for Yüzeyden 2 m. The calculations take into account the terrain (elevation), but with lower resolution than in reality. Therefore the models cannot differentiate, for instance, the temperature on a mountain peak or on a city square scorched by the sun. The general rule is that the centres of large cities are 1 °C to 3 °C warmer than the surrounding area or natural landscapes. Significant temperature differences over a small area are primarily caused in the winter by an inversion. A short yet noticeable cooling can also occur after a local summer storm.