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    Températures
    Température ressentie
    Précipitations
    Radar
    Satellite
    Nuages
    Vitesse du vent
    Rafales
    Pression atm.
    Orages
    Humidité
    Mer
    Enneigement
    Pollution de l'air
    DémarrerPrécédentSuivantChanger la dateAujourd'hui, 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
    lumamejevesadi
    24252627282930
    31mars010203040506
    07080910111213

    Données : HRRR, NOAA (résolution 3 km)
    Mise à jour : 20:00 UTC (prochaine mise à jour : 21:00 UTC - préparé)
    Heure actuelle : 22:00, 26/03/2025 (UTC)

    For this output data, temperature is shown for 2 m au-dessus du sol. 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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