Данни: ICON, DWD (резолюция 7 km)
Обновено: 09:00 UTC (следващо обнов.: 12:00 UTC - подготви)
Текущо време: 16:00, 08.04.2025 (UTC)

For this output data, temperature is shown for 2 м над земята. 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.