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  • New High-Resolution NAM Model Now Available for the U.S. and Hawaii NAM

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    Temperatura
    Temperatura percepita
    Precipitazioni
    Radar
    Satellite
    Nuvolosità
    Velocità del vento
    Raffiche di vento
    Pressione atmosferica
    Temporali
    Umidità
    Mare
    Manto nevoso
    Inquinamento atmosferico
    AvviaPrecedenteSuccessivoCambia dataOggi, 26/03/202500:0001:0002:0003:0004:0005:0006:0007:0008:0009:0010:0011:0012:0013:0014:0015:0016:0017:0018:0019:0020:0021:0022:0023:00
    lumamegivesado
    24252627282930
    31marzo010203040506
    07080910111213

    For this output data, temperature is shown for 2 m sopra il suolo. 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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    中浜海岸4.6k
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