| Mjesto | D2 Blučina - Prognoza |
| Pruža | dopravniinfo.cz |
| Smjer | sjever |
● D2 Nosislav 2 km dopravniinfo.cz
● Židlochovice 5 km zidlochovice.cz
● D2 Rajhradice 6 km dopravniinfo.cz
● Hustopeče 11 km fair-net.eu
● Chrlice 12 km dopravniinfo.cz
● Brno-jih 15 km dopravniinfo.cz
Podaci: ICON, DWD (razlučivost 7 km)
Ažurirani: 15:00 UTC (sljedeće ažuriranje: 18:00 UTC - pripremi)
Vrijeme sad: 21:00, 23.03.2025 (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.