Condensation

Condensation is the process by which water vapor in the air is changed into liquid water. This is the opposite of evaporation. Condensation generally occurs when the air is cooled to its dew point, or when it becomes saturated with water vapor. When the temperature drops to the dew point, the air is unable to hold all the moisture, causing it to condense into liquid form. This process is responsible for the formation of clouds, fog, dew, and frost. In the water cycle, condensation plays a crucial role in returning water from the atmosphere back to the Earth’s surface. It also releases heat into the atmosphere, which can lead to further atmospheric changes and phenomena.