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

    University of Arizona campus from the Computer Science offices in the Gould-Simpson building

    University of Arizona campus from the Computer Science offices in the Gould-Simpson building - Web-kamere
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    Mjesto University of Arizona campus from the Computer Science offices in the Gould-Simpson building - Prognoza
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    Jučer & Danas

    University of Arizona campus from the Computer Science offices in the Gould-Simpson building - Jučer
    Jučer
    University of Arizona campus from the Computer Science offices in the Gould-Simpson building - Danas
    Danas
    Usporedba slike od zadnje dostupno vrijeme (desno) sa slikom od prije 24 sata (lijevo).

    Najbliže web kamere

    South Tucson 3 km simplybits.net

    I-10 WB 259.40 @22nd St 3 km az511.com

    I-10 EB 256.20 @Grant Rd 4 km az511.com

    I-10 WB 260.10 @I-19 5 km az511.com

    Temperatura
    Osjet ugode
    Padaline
    Radar
    Satelit
    Oblaci
    Brzina vjetra
    Udari vjetra
    Tlak zraka
    Grmljavinska oluja
    Vlaga
    More
    Snježni pokrivač
    Onečišćavanje zraka
    ReproducirajNatragDaljePromijeni datumDanas, 21.03.202500:0001:0002:0003:0004:0005:0006:0007:0008:0009:0010:0011:0012:0013:0014:0015:0016:0017:0018:0019:0020:0021:0022:0023:00
    poutsrčepesune
    17181920212223
    24252627282930
    31ožujak010203040506

    Podaci: HRRR, NOAA (razlučivost 3 km)
    Ažurirani: 13:00 UTC (sljedeće ažuriranje: 14:00 UTC - pripremi)
    Vrijeme sad: 15:00, 21.03.2025 (UTC)

    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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