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Waters from the tropics follow this trunk route north and then east into the North Atlantic. |
Cold Arctic waters make their way southward into the Atlantic. |
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The northern extension of the Gulf Stream warms the coasts of Iceland, Norway, and Spitsbergen. |
The Pacific twin of the East Greenland Current is heavy with the cold waters moving south from the Bearing Sea. |
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The northernmost arm of the Gulf Stream brings warmish waters to meet the cold of the Arctic Ocean. |
A wide, cold and sluggish current follows the west coast of the U.S. as far as Baja California. |
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"The black current," Pacific's equivalent of the Atlantic's Gulf Stream, brings dark tropical waters up past Japan. |
Cold waters and iceburgs are brought down from Baffin Bay and meet the warm Gulf Stream off Newfoundland, producing the fogs of the Grand Banks. |
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In June and August, during the Southwest Monsoon, the Somali current flows north, but during the winter it reverses dirction. |
The Benguela current drives water northward and westward into midocean. This produces a strong upwelling of water and nutrients from the ocean bed, supporting enormous numbers of fish. |
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The strongest north-south current in the southern hemisphere stays close to the coast of southern Africa. 7. South
Equatorial Current
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A cold current brings nutrients to the sea surface, which teems with life. Every ten years or so, complex weather conditions strengthen the warm, eastward-flowing Equatorial Countercurrent. The Humboldt Current is disrupted. The nutrients no longer rise from the ocean depths, and fish starve. Peruvian fisherman have called this disasterous phenomenom El Nino ("the child") because of it's occurence around Christmas. |
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The Pacific equivalent of the North Atlantic Drift brings the warm waters of the Kuroshio to the coast of Africa. |
The greatest current of all is driven by the Westerlies. It circles the Antarctic continent, traveling at about half a mile an hour around the Southern Ocean. |
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The Trade Winds build up water on the western side of the oceans; the Equatorial Counter-current flows eastward, restoring the balance. |
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The extension of the Atlantic Equatorial Countercurrent was used by Portuguese explorers sailing down the coast of Africa. |