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Humidity
The amount of water vapor in the atmosphere varies from place to place. Humidity is the term used to describe the amount of water vapor in the atmosphere.
Water vapor
Relative humidity the exact amount of water vapor in the atmosphere (specific humidity)
Water is stored in the atmosphere in the form of water vapor.
Humidity
Meteorologists study the dew point because it is the basic measure of the state of the atmosphere. The dew point tells scientists how much water vapor is in the air.
vapor
The amount of water vapor in the atmosphere varies from place to place. Humidity is the term used to describe the amount of water vapor in the atmosphere.
The main processes that return water vapor to the atmosphere are evaporation and transpiration. Evaporation occurs when liquid water changes into water vapor from sources such as oceans, lakes, and rivers. Transpiration is the process through which plants release water vapor from their leaves into the atmosphere. Both of these processes contribute to the water cycle by replenishing the atmosphere with water vapor.
Water vapor
Relative humidity the exact amount of water vapor in the atmosphere (specific humidity)
Water is stored in the atmosphere in the form of water vapor.
Water vapor
Water vapor
The stratosphere contains almost no water vapor.
The process of which water is stored in the atmosphere as vapor, such as clouds & humidity.