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Podaci: HRRR, NOAA (razlučivost 3 km)
Ažurirani: 16:00 UTC (sljedeće ažuriranje: 17:00 UTC - pripremi)
Vrijeme sad: 18:00, 23.04.2025 (UTC)
For this output data, temperature is shown for 2 m iz. nad. vis.. 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.