Najbliže web kamere
● Petrov 0 km batak.cz
● Sudoměřice 2 km pocasi-sudomerice.cz
● Veselí nad Moravou 10 km batak-live.cz
● Hodonín 11 km hodonin.eu
● Šibenica 13 km letiskoholic.sk
● Vřesovice 20 km vresovicepocasi.cz
● Petrov 0 km batak.cz
● Sudoměřice 2 km pocasi-sudomerice.cz
● Veselí nad Moravou 10 km batak-live.cz
● Hodonín 11 km hodonin.eu
● Šibenica 13 km letiskoholic.sk
● Vřesovice 20 km vresovicepocasi.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.