Earth's orbital changes, influenced by Milankovitch cycles, have significant impacts on climate patterns and temperature variations.
The changes in Earth's orbit, including an increased angle of rotation axis and shift from circular to elliptical orbit, have significant impacts on Earth's climate. These changes, known as Milankovitch cycles, influence the amount of solar radiation reaching Earth, affecting temperature variations and climate patterns over long periods.
Increased angle of axis of rotation: This change impacts the distribution of sunlight on Earth's surface, influencing seasonal temperature variations. Increased elliptical orbit closer to the sun: Moving closer to the sun in an elliptical orbit can lead to warmer climates due to increased solar radiation. Consistent circular orbit: A circular orbit results in milder summers and winters, leading to little variation in temperatures.
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