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The three components of the Milankovitch theory are eccentricity (changes in Earth's orbit shape), axial tilt (variation in the angle of Earth's axis), and precession (wobbling of Earth's axis orientation). These factors influence the amount and distribution of solar radiation reaching Earth, contributing to long-term climate changes.

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Milutin Milanković was a Serbian mathematician, astronomer, and geophysicist known for his work on the mathematical theory of climate and the study of Earth's long-term climate variations. He proposed the theory of changes in Earth's orbit and tilt as the key drivers of ice ages in what is known as the Milankovitch cycles. His work revolutionized the understanding of Earth's past climate changes.


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