Water vapour forms clouds that bring rain.
The important source of water vapor in the atmosphere is evaporation from the Earth's surface, primarily from oceans, lakes, and rivers. This process involves the conversion of liquid water into water vapor due to the Sun's energy.
Wetness in the atmosphere refers to the presence of water vapor. It is essential for processes like cloud formation and precipitation. Water vapor is an important component of Earth's atmosphere and plays a key role in regulating the planet's climate.
Water vapor is added to the atmosphere primarily by evaporation from bodies of water such as oceans, lakes, and rivers. Evapotranspiration from plants also contributes to the amount of water vapor in the atmosphere.
Evaporation, where water on the Earth's surface turns into water vapor, and transpiration, where plants release water vapor through their leaves, both add water vapor to the atmosphere.
The layer of the atmosphere that contains the most water vapor is the troposphere, the lowest layer of the atmosphere where most weather phenomena occur. Water vapor concentration decreases with height in the atmosphere as temperature decreases.
The important source of water vapor in the atmosphere is evaporation from the Earth's surface, primarily from oceans, lakes, and rivers. This process involves the conversion of liquid water into water vapor due to the Sun's energy.
Water Vapor
Wetness in the atmosphere refers to the presence of water vapor. It is essential for processes like cloud formation and precipitation. Water vapor is an important component of Earth's atmosphere and plays a key role in regulating the planet's climate.
vapor
Water vapor is added to the atmosphere primarily by evaporation from bodies of water such as oceans, lakes, and rivers. Evapotranspiration from plants also contributes to the amount of water vapor in the atmosphere.
The evaporation is less important if the atmosphere is humid.
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.
Evaporation, where water on the Earth's surface turns into water vapor, and transpiration, where plants release water vapor through their leaves, both add water vapor to the atmosphere.
Just as the Earth's Nitrogen cycle and its Carbon cycle are cyclic, the Earth's Water Cycle is just that; Water Vapor returns to the Atmosphere to complete the Cycle.
Water vapor
Water vapor
The layer of the atmosphere that contains the most water vapor is the troposphere, the lowest layer of the atmosphere where most weather phenomena occur. Water vapor concentration decreases with height in the atmosphere as temperature decreases.