Uneven heating by the sun generates atmospheric patterns, influencing climate and weather phenomena.
Uneven heating of the Earth's surface by the Sun leads to differential heating, causing air to rise in warm regions and sink in cooler areas. This creates pressure gradients, initiating wind flows and atmospheric circulation.
Curvature of the Earth also plays a role in uneven heating, with energy surplus at the equator and deficit at the poles. Weather acts to transfer this excess energy toward the poles, creating a balance.
Solar radiation powers environmental processes, influencing temperature, wind, moisture, and ultimately shaping climate, landforms, and weather phenomena like hurricanes and wind patterns.
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