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  2. Humidity - Wikipedia

    en.wikipedia.org/wiki/Humidity

    Humidity depends on the temperature and pressure of the system of interest. The same amount of water vapor results in higher relative humidity in cool air than warm air. A related parameter is the dew point. The amount of water vapor needed to achieve saturation increases as the temperature increases.

  3. Dew point - Wikipedia

    en.wikipedia.org/wiki/Dew_point

    If all the other factors influencing humidity remain constant, at ground level the relative humidity rises as the temperature falls; this is because less vapor is needed to saturate the air. In normal conditions, the dew point temperature will not be greater than the air temperature, since relative humidity typically [5] does not exceed 100%. [6]

  4. Psychrometrics - Wikipedia

    en.wikipedia.org/wiki/Psychrometrics

    The dew point temperature is measured easily and provides useful information, but is normally not considered an independent property of the air sample as it duplicates information available via other humidity properties and the saturation curve. Relative humidity (RH) is the ratio of the mole fraction of water vapor to the mole fraction of ...

  5. Wet-bulb temperature - Wikipedia

    en.wikipedia.org/wiki/Wet-bulb_temperature

    The wet-bulb temperature is the lowest temperature that may be achieved by evaporative cooling of a water-wetted, ventilated surface.. By contrast, the dew point is the temperature to which the ambient air must be cooled to reach 100% relative humidity assuming there is no further evaporation into the air; it is the temperature where condensation (dew) and clouds would form.

  6. Vapor pressure - Wikipedia

    en.wikipedia.org/wiki/Vapor_pressure

    Graph of water vapor pressure versus temperature. At the normal boiling point of 100 ... Relative humidity is defined relative to saturation vapor pressure. [18]

  7. Density of air - Wikipedia

    en.wikipedia.org/wiki/Density_of_air

    The saturation vapor pressure of water at any given temperature is the vapor pressure when relative humidity is 100%. One formula is Tetens' equation from [15] used to find the saturation vapor pressure is: = ⁡ (()) where:

  8. Water vapor - Wikipedia

    en.wikipedia.org/wiki/Water_vapor

    At max. saturation (i. e. rel. humidity = 100% at 0 °C) the density will go down to 28.51 g/mol. STP conditions imply a temperature of 0 °C, at which the ability of water to become vapor is very restricted. Its concentration in air is very low at 0 °C. The red line on the chart to the right is the maximum concentration of water vapor ...

  9. Lifting condensation level - Wikipedia

    en.wikipedia.org/wiki/Lifting_condensation_level

    The LCL can be either computed or determined graphically using standard thermodynamic diagrams such as the skew-T log-P diagram or the tephigram.Nearly all of these formulations make use of the relationship between the LCL and the dew point, which is the temperature to which an air parcel needs to be cooled isobarically until its RH just reaches 100%.

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