the amount of humidity in the atmosphere is the measure of (_) in air
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1.5 Atmospheric humidity. Atmospheric humidity is the amount of water vapor carried in the air. It can be measured as vapor pressure, mixing ratio or specific humidity. Specific humidity is the ratio of vapor mass to total air mass, whereas mixing ratio is the ratio of the mass of vapor to the mass of dry air.
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The most commonly used measure of humidity is relative humidity. Relative humidity can be simply defined as the amount of water in the air relative to the saturation amount the air can hold at a given temperature multiplied by 100.
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