A Rossby wave is a type of wave that occurs in rotating fluids, such as the Earth's atmosphere and oceans, due to the Coriolis effect. These waves are significant in meteorology and oceanography because they play a crucial role in the motion of weather systems and ocean currents. In the atmosphere, Rossby waves are characterized by large-scale meanders in high-altitude winds, particularly in the westerlies, and are influenced by the planet's rotation.
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