Humidity in daily life means relative humidity. Relative humidity is the partial pressure of water vapor in the air of a particular place and the saturated vapor pressure of water vapor at that temperature. The amount of water vapor in the air of a place is indicated by the amount of dry or wet humidity in the air. * Dew point: The ability of air to hold water vapor of a certain volume at a certain temperature is limited. As the temperature rises, the water vapor holding capacity of the place increases When the temperature of a place decreases, the water vapor holding capacity of that place decreases As the temperature gradually decreases, the atmosphere at a certain temperature is saturated by the water vapor of the place. At that temperature, the water vapor in the air then turns into dew This temperature is dew point