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Equatorial Countercurrent

   Also found in: Wikipedia 0.03 sec.
Equatorial Countercurrent [‚e·kwə′tȯr·ē·əl ′kau̇nt·ər‚kər·ənt]
(oceanography)
An ocean current flowing eastward (counter to and between the westward-flowing North Equatorial Current and South Equatorial Current) through all the oceans.


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Off the equator, subsurface propagation of anomaly patterns initiates an SST anomaly in the North Equatorial Countercurrent regions of the western Pacific, which then intensifies and moves into the equatorial waveguide, consistent with the mean water pathways found above.
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.
Retroflection eddies appear to carry a significant volume of South Atlantic water northward into the North Atlantic, short-circuiting the longer route around the gyre formed by the North Equatorial Countercurrent and the North Equatorial Current.
 
 
 
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