The humidity of the atmosphere is measured with the help of a Hygrometer, also known as
Dry and Wet Bulb Thermometer. In the Dry and Wet Bulb Thermometer, a piece of wet cloth is tied around one bulb, the other end of the cloth dips into a small container of water. The rate
of evaporation of water vapour from the wet bulb keeps the temperature of this bulb lower
than the dry bulb. A difference in temperature between the two thermometers indicates the
relative humidity. Saturated air will not allow evaporation and in that case the temperature reading on both the dry and wet thermometers will be the same. This would mean that Relative
Humidity is 100%.
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