The continuous movement of water on, above, and below the surface of the Earth is described by the water cycle, also known as the hydrologic cycle. Evaporation, condensation, precipitation, and runoff are just a few of the crucial processes that make up the cycle.
Water vapor is created when heat energy is absorbed during the process of evaporation, which turns water from a liquid to a gas. Although it also happens from the surface of the soil and vegetation, this mostly happens at the surface of bodies of water, such as oceans, lakes, and rivers. Temperature, humidity, wind speed, and the amount of water surface area available for evaporation are just a few of the variables that affect how much water evaporates.
In order to form clouds, water vapor cools as it ascends and eventually condenses into tiny droplets. These clouds have the ability to produce precipitation, such as rain, snow, or hail, which replenishes the water on the Earth's surface. When the water enters rivers, streams, and oceans, the cycle restarts.
Since it helps to distribute water throughout the Earth's atmosphere and regulates the planet's temperature, evaporation is a crucial component of the water cycle. It is also a crucial process in agriculture because it enables plants to absorb water through their roots and transfer it to their leaves for photosynthesis.