The degree of saturation can also be expressed as:
μ = φ (p a - p ws ) / (p a - p w ) (2)
μ = degree of saturation
φ = relative humidity (%)
p w = vapor pressure (mbar)
p ws = saturation vapor pressure at the actual dry bulb temperature (mbar)
p a = atmospheric pressure of moist air (mbar)
Moist and humid air - psychrometric charts, Mollier diagrams, air-condition temperatures and absolute and relative humidity and moisture content.
Relative humidity in moist air can estimated by measuring the dry and wet bulb temperature.
The mass of water vapor present in moist air - to the mass of dry air.
Maximum water content in humid air vs. temperature.
The moisture holding capacity of air increases with temperature.
Saturation pressure and maximum water content in compressed air.
Dry Bulb, Wet Bulb and Dew Point temperatures can be used to determine the state of humid air.
Pressure, temperature and volume in a perfect ideal gas like moist air (air with water vapor).
The pressure in a mixture of dry air and water vapor - humid or moist air - can be estimated by using Daltons Law of partial pressures.
Density of the mix of dry air and water vapor - moist humid air.
Sensible and latent heat of moist air.
Psychrometric table with humid air properties like saturation pressure, specific volume, enthalpy and entropy.
Relative humidity in moist air is the ratio of partial vapor pressure to air pressure.
Saturation pressure of water vapor in moist air vs. temperature.
Online calculator, figures and tables with water saturation (vapor) pressure at temperatures ranging 0 to 370 °C (32 to 700°F) - in Imperial and SI Units.
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