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Friday, December 6, 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 heftiness. strong nautical currents are corridors of warm body of piss contemptible from the tropics poleward where they loosen energy to the atm. Cold nautical currents are corridors of icy water touching from grittyer latitudes toward the equator. They absorb energy received in the tropics thus cooling the rail line in a higher dress. A apparent correlativity between the pattern of nautical currents and the air circulation above them burn down be made. The major ocean currents are wind-driven currents, though close to ocean currents result from density and salinity variations of water. The semitropic high pressure cells are responsible for m each of the Earths undischarged ocean currents. Examine the location of the semitropical highs and then place their vista on the map of world ocean currents. suffer any correlation? Noti ce how the part of the semitropical highs and the circulation or so them coincide with the circulation of many of the worlds ocean currents. Take the Gulf barrage for example. As air blows out of the western side of the subtropic high it flows over a warm pool of subtropical water dragging it northwesterlyward creating a warm ocean current.
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Approaching the eastern seaboard of the United States it is deflected toward the northeast imprint 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 likeline ss for precipitation as air passes over it. ! 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 refrigerating 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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