Milutin Milanković was a Serbian geophysicist and astronomer who, in the 1920s, calculated what has become known as the Milankovitch Cycle, describing the collective effects of changes in the Earth’s movements on its climate millions of years. He hypothesized that variations in eccentricity, axial tilt, and precession combined, creating cyclical variations in the intra-annual and latitudinal distribution of solar radiation on the Earth’s surface. This cycle has greatly influenced climate, resulting in major climatic patterns.
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