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What Is the Difference Between Relative Humidity and Dew Point?
Relative humidity and dew point are two different ways of measuring the amount of water content in the air. The relative humidity is the percentage of water content in the air, relative to the maximum the air can hold at a given temperature. The relative humidity changes when the air temperature changes because warmer air can hold more water content than cooler air.
The dew point is an absolute measure of water content, independent of air temperature. When relative humidity reaches 100% and cannot hold more water content, this temperature is called the dew point.
How Do You Calculate Dew Point?
Dew point temperature can be calculated using Td = T - [(100 - RH)/5]. In degrees Celsius, Td is dew point temperature, T is observed temperature, and RH is the relative humidity. This formula was proposed in the February 2005 Bulletin of the American Meteorological Society by Mark G. Lawrence and is accurate for relative humidity values above 50%.
The dew point is the temperature, pressure, and humidity level that causes water vapor contained in the air to condense into liquid form.
Wayne Groszko
Wayne Groszko is a consultant, researcher, and teacher in Energy Sustainability with 13 years of experience. He has taught at Dalhousie University and the Nova Scotia Community College, in the Faculties of Engineering, Environmental Science, and Energy Sustainability Engineering Technology. Wayne is also President of the Community Energy Cooperative of New Brunswick, and has worked as Renewable Energy Coordinator with the Ecology Action Centre in Nova Scotia. He holds a B.Sc. (Hon.) from the University of Calgary, and a Ph.D. from Dalhousie University.