dew point

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Geliefert zwischen Mi., 04.02.2026 und Do., 05.02.2026

Details

The dew point is the temperature to which a given parcel of air must be cooled, at constant barometric pressure, for water vapor to condense into water. The condensed water is called dew. The dew point is a saturation point.The dew point is associated with relative humidity. A high relative humidity indicates that the dew point is closer to the current air temperature. Relative humidity of 100% indicates the dew point is equal to the current temperature and the air is maximally saturated with water. When the dew point remains constant and temperature increases, relative humidity will decrease.At a given barometric pressure, independent of temperature, the dew point indicates the mole fraction of water vapor in the air, and therefore determines the specific humidity of the air. The dew point is an important statistic for general aviation pilots, as it is used to calculate the likelihood of carburetor icing and fog, and estimate the height of the cloud base.

Weitere Informationen

  • Allgemeine Informationen
    • GTIN 09786130838645
    • Editor Frederic P. Miller, Agnes F. Vandome, John McBrewster
    • Genre Physik & Astronomie
    • EAN 9786130838645
    • Format Fachbuch
    • Titel dew point
    • Herausgeber Alphascript Publishing
    • Anzahl Seiten 76

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