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    Temperatura
    Osjet ugode
    Padaline
    Radar
    Satelit
    Oblaci
    Brzina vjetra
    Udari vjetra
    Tlak zraka
    Grmljavinska oluja
    Vlaga
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    Snježni pokrivač
    Onečišćavanje zraka
    ReproducirajNatragDaljePromijeni datumDanas, 30.03.202500:0001:0002:0003:0004:0005:0006:0007:0008:0009:0010:0011:0012:0013:0014:0015:0016:0017:0018:0019:0020:0021:0022:0023:00
    poutsrčepesune
    24252627282930
    31ožujak010203040506
    07080910111213

    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.

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