This collects data for weather, climate, and environmental monitoring from space
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Air Masses or Bodies of air
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This is called relative humidity. It is the ratio between the actual humidity, and the humidity for saturated air - that is, the maximum amount of water air can hold. This saturation point is dependent on temperature.
The measurement of the grams of water in a kilogram of air is called specific humidity.
When the air temp drops to the dew point that is 100% relative humidity - the air is saturated and condensation willf form. In general, the air temp cannot drop below the dew point so humidities greater than 100% do not occur.