Data: ICON, DWD (resolusi 7 km)
Diperbarui: 09:00 UTC (pembaruan selanjutnya: 12:00 UTC - persiapan)
Waktu sekarang: 14:00, 25/04/2025 (UTC)

For this output data, temperature is shown for 2 m di atas tanah. 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.