![]() Wind
Wind develops as a result of pressure or temperature differences between two locations on the Earth's surface. Sea breezes for example, develop due to the differential heating of land and sea at the coast during warm sunny days. Winds also blow out from high-pressure regions or anticyclones and into low-pressure regions, for example depressions. The wind however, does not blow in a straight line, but follows a spiralling path because large movements of air are deflected by the Coriolis force as a result of the Earth's rotation. At a global scale, the temperature and pressure differences across the latitudes of the Earth generate the global wind belts. |
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