Najbliže web kamere
● Kývalka 2 km dopravniinfo.cz
● Panská horka 7 km gcm.cz
● Panská horka 7 km lsbyc.cz
● Brněnská přehrada 8 km kamera.nafleku.cz
● Zbýšov 8 km pocasizbysov.info
● Padochov 9 km meteopadochov.eu
● Kývalka 2 km dopravniinfo.cz
● Panská horka 7 km gcm.cz
● Panská horka 7 km lsbyc.cz
● Brněnská přehrada 8 km kamera.nafleku.cz
● Zbýšov 8 km pocasizbysov.info
● Padochov 9 km meteopadochov.eu
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.