The Water Cycle Explained

The Water Cycle Explained



The water cycle, also known as the hydrological cycle, is the continuous movement of water within the Earth and atmosphere. It involves several key processes: evaporation, condensation, precipitation, infiltration, and runoff.

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The cycle begins with evaporation, where water from oceans, rivers, and lakes is heated by the sun, transforming into vapor and rising into the atmosphere. This vapor cools and condenses to form clouds through the process of condensation. When the clouds become heavy enough, precipitation occurs, resulting in rain, snow, sleet, or hail falling back to the Earth's surface.

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Once the precipitation reaches the ground, it can either infiltrate into the soil, replenishing groundwater supplies, or flow over the surface as runoff, eventually returning to bodies of water like rivers and oceans. This process ensures that ecosystems receive the necessary moisture to thrive.

 

The water cycle is essential for maintaining life, regulating climate, and supporting natural processes. It illustrates the interconnectedness of Earth’s systems and highlights the importance of water conservation. Understanding the water cycle helps us appreciate the vital role water plays in sustaining the environment and human life.


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