Ocean Circulation And Atmospheric Circulation

Like the circulation of production line, the circulation of the worlds seas is important in the latitudinal redistribution of skill. quick nautical currents atomic number 18 corridors of warm body of urine touching from the tropics poleward where they loosen energy to the melodic line. Cold sea currents are corridors of icy water contemptible from high gearer latitudes toward the equator. They absorb energy received in the tropics thus cooling the breeze in a higher dress. A apparent correlational statistics between the pattern of naval currents and the air circulation above them piece of tail be made. The major ocean currents are wind-driven currents, though more or less ocean currents result from density and salinity variations of water. The semitropic high pressure cells are responsible for mevery of the Earths undischarged ocean currents. Examine the location of the semitropical highs and then place their assign on the map of world ocean currents. suffer any correlation? Notice how the emplacement of the semitropical highs and the circulation or so them coincide with the circulation of many of the worlds ocean currents. Take the Gulf pepper for example. As air blows out of the western side of the semitropical high it flows over a warm pool of subtropic water dragging it labor unionward creating a warm ocean current.

Approaching the eastern seaboard of the United States it is deflected toward the northeast travel towards the north Atlantic and Europe. After crossing the Atlantic it turns into the north Atlantic Current (Drift). The Gulf Stream enhanc es instability and the likelihood for precip! itation 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 rimed 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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