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Coriolis force |
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Coriolis force [ˌkɒrɪˈəʊlɪs] n (Astronomy) a fictitious force used to explain a deflection in the path of a body moving in latitude relative to the earth when observed from the earth. The deflection (Coriolis effect) is due to the earth's rotation and is to the east when the motion is towards a pole [named after Gaspard G. Coriolis (1792-1843), French civil engineer]
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