Nearest webcams
● Holešov 0 km drasal.cz
● Koupaliště Holešov 1 km koupaliste-holesov.cz
● Holešov 1 km chmi.cz
● Prusinovice 5 km vesani.cz
● Ski Areál Rusava 8 km webcamlive.cz
● Zlín 12 km webcamlive.cz
● Holešov 0 km drasal.cz
● Koupaliště Holešov 1 km koupaliste-holesov.cz
● Holešov 1 km chmi.cz
● Prusinovice 5 km vesani.cz
● Ski Areál Rusava 8 km webcamlive.cz
● Zlín 12 km webcamlive.cz
For this output data, temperature is shown for 2 m above ground. 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.