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The uneven heating of Earth's atmosphere is primarily caused by Earth's tilted axis, leading to varying climatic seasons.
The uneven heating of Earth's atmosphere is primarily caused by Earth's tilted axis. The tilt of the Earth's axis results in varying angles of direct sunlight, leading to different climatic seasons. This tilt causes regions near the equator to receive more direct sunlight and thus experience warmer temperatures, while areas near the poles receive less direct sunlight, resulting in colder temperatures.
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