The tilt of Earth's axis, shape of Earth's orbit, and distance from the Sun influence the cycle of seasons on Earth.
Earth's cycle of seasons is primarily caused by the tilt of Earth's axis, which results in varying amounts of sunlight reaching different parts of the Earth throughout the year. This tilt affects the intensity of solar radiation received at different latitudes, leading to changes in temperature and weather patterns.
Additionally, changes in the shape of Earth's orbit and the distance between Earth and the Sun also play a role in influencing the amount of solar energy Earth receives, contributing to seasonal variations.
Overall, these factors interact to create the distinctive patterns of seasons observed on Earth, demonstrating the intricate relationship between Earth's position in its orbit and the changing climate.
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