| Mjesto | Jabloňov - D1 - Prognoza |
| Pruža | dopravniinfo.cz |
| Smjer | jugoistok |
● Velké Meziříčí - D1 4 km dopravniinfo.cz
● Velké Meziříčí 5 km unet.cz
● Aeroklub Křižanov 5 km lkka.cz
● Aeroklub Křižanov 5 km lkka.cz
● Velké Meziříčí 5 km velkemezirici.cz
● Náměšť nad Oslavou 15 km sportvnamesti.cz
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.