Atmospheric Circulation
Atmospheric circulation refers to the large-scale movement of air around the Earth, driven by differences in temperature and pressure. This circulation is responsible for the weather patterns we experience, and is influenced by a variety of factors including the rotation of the Earth, the distribution of land and water, and the heating and cooling of the atmosphere. In the maritime context, atmospheric circulation plays a crucial role in determining wind patterns and ocean currents, which in turn affect navigation, shipping routes, and weather forecasting.
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