The water cycle in nature, also known as the hydrological cycle, describes the continuous movement of water on, above, and below the surface of the Earth. It involves processes such as evaporation, condensation, precipitation, and runoff.
Here's a brief explanation of the water cycle:
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Evaporation: The sun heats up water bodies like oceans, rivers, and lakes, causing water to evaporate and rise into the atmosphere in the form of water vapor.
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Condensation: As the water vapor rises, it cools and condenses to form clouds in the atmosphere.
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Precipitation: When the clouds become saturated with water, precipitation occurs in the form of rain, snow, sleet, or hail, bringing water back to the Earth's surface.
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Runoff: The precipitation that falls on the land can flow over the surface as runoff, eventually making its way back to oceans, rivers, and lakes, where the cycle begins again.
This continuous cycle of evaporation, condensation, precipitation, and runoff is essential for the distribution of water across the planet and plays a crucial role in sustaining life on Earth.
