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Air Humidity Ratio

The ratio between the mass of water vapor present in moist air - to the mass of dry air

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The humidity ratio of moist air can be expressed with

  • the mass of water vapor in the humid air - to the mass of dry air, or by
  • the partial pressure of vapor in the air - to the partial pressure of the dry air

Humidity Ratio by Mass

Humidity ratio by mass can be expressed as

  • the ratio between the actual mass of water vapor present in moist air - to the mass of the dry air

Humidity ratio is normally expressed in kilograms (or pounds) of water vapor per kilogram (or pound) of dry air.

Humidity ratio expressed by mass:

x = mw / ma                                  (1)


x = humidity ratio (kgwater/kgdry_air, lbwater/lbdry_air)

mw = mass of water vapor (kg, lb)

ma = mass of dry air (kg, lb)

Humidity Ratio by Vapor Partial Pressure

Based on the Ideal Gas Law the humidity ratio can be expressed as

x = 0.62198 pw / (pa - pw)                            (2)


pw = partial pressure of water vapor in moist air (Pa, psi)

pa = atmospheric pressure of moist air (Pa, psi)

The maximum amount of water vapor in the air is achieved when pw = pws the saturation pressure of water vapor at the actual temperature. (2) can be modified to:

xs = 0.62198 pws / (pa - pws)                                (3)


xs = maximum saturation humidity ratio of air (kgwater/kgair, lbwater/lbdry_air)

pws = saturation pressure of water vapor

The water vapor pressure is small regarding to the atmospheric pressure and the relation between the humidity ratio and the saturation pressure is almost linear.

Note! - be careful with these equations at higher temperatures - as indicated in Temperature and Moisture Holding Capacity of Air.

Maximum specific humidity at some common temperatures:

Water Vapor
Saturation Pressure

Maximum Saturation
Humidity Ratio of Air
- x -
0 609.9 0.003767
5 870 0.005387
10 1225 0.007612
15 1701 0.01062
20 2333 0.014659
25 3130 0.019826
30 4234 0.027125

Moisture content vs. temperature in air diagram

Note that the saturation pressure of water vapor, - and the maximum humidity ratio, increases dramatically with air temperature. This important for the capacity of drying processes.

Example - Humidity Ratio of Moist Air

The humidity ratio for saturated moist air at 20oC with water vapor partial pressure 2333 Pa at atmospheric pressure of 101325 Pa (1013 mbar, 760 mmHg) can be calculated as:

x = 0.62198 (2333 Pa) / ((101325 Pa) - (2333 Pa))

= 0.0147 (kg/kg)

= 14.7 (g/kg)

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  • de: spezifische Feuchte Luftverhältnis gpp
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