The Science of Rainfall

Rainfall is a crucial component of the Earth’s water cycle and a fundamental natural process that sustains life. It begins with the evaporation of water from oceans, rivers, lakes, and other bodies of water, driven by the sun’s energy. This water vapor rises into the atmosphere, where it cools and condenses to form clouds. When the atmospheric conditions are right, these water droplets combine to form larger droplets, becoming heavy enough to fall to the ground as rain.

Formation of Rain

Rain formation involves several key steps:

  1. Evaporation: Water from the Earth’s surface evaporates into the atmosphere due to solar heat.
  2. Condensation: As the water vapor rises, it cools and condenses around tiny particles in the air, such as dust, pollen, or sea salt, forming clouds.
  3. Coalescence: Within the clouds, water droplets collide and merge to form

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Imran

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