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Relative Humidity

 

 

Relative Humidity is the most commonly used measurment of water vapor in the air. It doesn't actually tell us the amount of water vapor in the air but instead tells us how close the air is to being saturated. The relative humidty (RH) with respect to water is the ratio (expressed as a percentage) of the vapor pressure (e) to the saturation vapor pressure (es).

A relative humidty of more than 100% indicates air that is supersaturated. 

© 2015 by UniMet.

* All information on this site has come from lecture notes and the associated course text books: 'Atmospheric Science: An introductory survey, 2nd edition, J. M. Hobbs and P. V. Wallace' and 'Meteorology Today: An Introduction to Weather, Climate and the Environment, 10th edition (International), C. D. Ahrens.' Some sections may have been rephrased and altered slightly but all content came from the above mentioned sources unless otherwise stated. 

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