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The shape of Earth's orbit, known as its eccentricity, influences the distance between the Earth and the Sun throughout the year. When the orbit is more elliptical, variations in distance can lead to greater seasonal temperature differences, potentially affecting global climate patterns. During periods when Earth is closer to the Sun, average global temperatures can rise, while a more distant position can result in cooler temperatures. These orbital changes occur over long time scales and are part of natural climate cycles, such as Milankovitch cycles, which can impact climate over thousands of years.

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