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South Equatorial Current

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South Equatorial Current [′sau̇th ‚ek·wə′tȯr·ē·əl ′kə·rənt]
(oceanography)
Any of several ocean currents, flowing westward, driven by the southeast trade winds blowing over the tropical oceans of the Southern Hemisphere and extending slightly north of the equator. Also known as Equatorial Current.

South Equatorial Current 

a warm surface current that flows east to west in the southern tropical latitudes of the world ocean. The South Equatorial Current originates as a result of the action of the trade winds. In the Pacific Ocean it is a continuation of the Peru (Humboldt) Current; in the Atlantic Ocean, of the Benguela Current; and in the Indian Ocean, of the West Australian Current. As these currents approach the equator and are deflected to the west, they become the South Equatorial Current.



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The South Equatorial Current is fed by the northern and southern Indian oceans, and by the Pacific Ocean through the Indonesian archipelago.
The barrier layer is maintained over the long term through freshening of the near-surface, warm pool by rainfall that is balanced by sporadic mixing with saltier waters transported by the South Equatorial Current from the central tropical and subtropical Pacific.
The diatoms creating the streak in the Pacific congregate and thrive at the convergence of the North Equatorial Countercurrent and the cooler, denser water of the South Equatorial Current sinking below it, the scientists assert.
 
 
 
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