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The Earth's orbit affects climate primarily through variations in the distance from the Sun and the angle at which sunlight strikes the planet, known as Milankovitch cycles. These cycles include changes in eccentricity (the shape of the orbit), axial tilt, and precession (the wobble of the Earth's axis). These orbital changes influence the distribution of solar energy received by the Earth, leading to shifts in climate patterns over long periods, such as the onset of ice ages or warmer interglacial periods. Consequently, these variations can significantly impact global temperatures, precipitation patterns, and seasonal changes.

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4mo ago

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