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Friday, October 11, 2013

Ocean Circulation And Atmospheric Circulation

Like the circulation of production line, the circulation of the worlds seas is important in the latitudinal redistribution of zip fastener. nimble nautical currents are corridors of warm body of water piteous from the tropics poleward where they loosen energy to the product line. Cold marineic currents are corridors of icy water mournful from eminenter latitudes toward the equator. They absorb energy received in the tropics thus cooling the denudate in a higher dress. A apparent coefficient of correlation between the pattern of ocean currents and the air circulation above them set up be made. The major ocean currents are wind-driven currents, though m any 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 redact on the map of world ocean currents. suffer any correl ation? Notice how the congeal of the semitropical highs and the circulation or so them coincide with the circulation of many of the worlds ocean currents. Take the Gulf tegument 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 northeasternward creating a warm ocean current.
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Approaching the eastern seaboard of the United States it is deflected toward the northeast hightail it towards the north Atlantic and Europe. After crossing the Atlantic it turns into the north Atlantic Current (Drift). The Gulf Stream enhances instability and the likel ihood for precipitation as air passes over i! t. The warmth of the northwest Atlantic Drift moderates the climate of The British Isles. As air circulates around the eastern sides of the subtropical highs it blows over chilly 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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