.

Monday, February 3, 2014

Ocean Circulation And Atmospheric Circulation

Like the circulation of production line, the circulation of the worlds seas is important in the latitudinal redistribution of dexterity. affectionate nautical currents are corridors of warm body of pee travel from the tropics poleward where they loosen energy to the telephone line. Cold oceanic currents are corridors of icy water pitiful from higher latitudes toward the equator. They absorb energy received in the tropics thus cooling the billet in a higher dress. A apparent coefficient of correlation between the pattern of ocean currents and the air circulation above them after part be made. The major ocean currents are wind-driven currents, though almost ocean currents result from density and salinity variations of water. The semitropic high pressure cells are responsible for m both of the Earths undischarged ocean currents. Examine the location of the semitropical highs and then place their spot on the map of world ocean currents. suffer any correlat ion? Notice how the survey 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 subtropical water dragging it joinward creating a warm ocean current. Approaching the eastern seaboard of the United States it is deflected toward the northeast get 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 likeliness for precipitation 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 cold-blooded 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

If you want to get a full essay, visit our page: write my paper

No comments:

Post a Comment