Ocean Circulation And Atmospheric Circulation

Like the circulation of production line, the circulation of the worlds seas is important in the latitudinal redistribution of talent. partial(p) nautical currents argon corridors of warm body of body of water wretched from the tropics poleward where they loosen energy to the occupation. Cold oceanic currents are corridors of icy water lamentable from full(prenominal)er latitudes toward the equator. They absorb energy received in the tropics thus cooling the wrinkle in a higher dress. A apparent correlation between the pattern of ocean currents and the air circulation above them washstand be made. The major ocean currents are wind-driven currents, though m any(prenominal) ocean currents result from density and salinity variations of water. The semitropic high pressure cells are responsible for many of the Earths undischarged ocean currents. Examine the location of the semitropical highs and then place their slur on the map of world ocean currents. suff er any correlation? Notice how the positioning of the semitropical highs and the circulation or so them coincide with the circulation of many of the worlds ocean currents. Take the Gulf rain buckets for example. As air blows out of the western side of the subtropic high it flows over a warm pool of subtropic water dragging it conglutinationward creating a warm ocean current.

Approaching the eastern seaboard of the United States it is deflected toward the northeast blend in towards the north Atlantic and Europe. After crossing the Atlantic it turns into the north Atlantic Current (Drift). The Gulf Stream enha nces instability and the likelihood for prec! ipitation as air passes over it. The warmth of the northwestward Atlantic Drift moderates the climate of The British Isles. As air circulates around the eastern sides of the subtropical highs it blows over wintry pools of water dragging them equatorward creating cold ocean currents. The Peru Current is a wind-driven cold current that flows along the coast of South America. Air moving over the cold current is stabilized, inhibiting uplift, the development of clouds and precipitation. Cool...If you want to position a full essay, order it on our website: OrderCustomPaper.com

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