Najbliže web kamere
● Padochov 1 km meteopadochov.eu
● Zbýšov 3 km pocasizbysov.info
● Ivančice 4 km meteo.mikroregion.online
● Budkovice 5 km czechheaven.cz
● Ostrovačice - D1 10 km dopravniinfo.cz
● Zbraslav u Brna 12 km pocasizbraslav.cz
● Padochov 1 km meteopadochov.eu
● Zbýšov 3 km pocasizbysov.info
● Ivančice 4 km meteo.mikroregion.online
● Budkovice 5 km czechheaven.cz
● Ostrovačice - D1 10 km dopravniinfo.cz
● Zbraslav u Brna 12 km pocasizbraslav.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.