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● Brno - Medlánky 3 km akmedlanky.cz
● Brno - Poříčí 4 km bkom.cz
● Brněnská přehrada 4 km kamera.nafleku.cz
● Brno 4 km brno.cz
● Panská horka 4 km gcm.cz
● Panská horka 4 km lsbyc.cz
● Brno - Medlánky 3 km akmedlanky.cz
● Brno - Poříčí 4 km bkom.cz
● Brněnská přehrada 4 km kamera.nafleku.cz
● Brno 4 km brno.cz
● Panská horka 4 km gcm.cz
● Panská horka 4 km lsbyc.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.