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The Equatorial Counter Current is an eastward flowing, wind-driven current which extends to depths of 100–150 metres (330–490 ft) in the Atlantic, Indian, and Pacific Oceans. More often called the North Equatorial Countercurrent (NECC), this current flows west-to-east at about 3-10°N in the Atlantic, Indian … See more
The NECC is a direct response to the meridional changes in the coriolis parameter and the wind stress curl near the Intertropical Convergence Zone (ITCZ). In part the NECC owes its existence to the fact that the ITCZ is … See more
The Pacific NECC is a major eastward moving surface current that transports more than 20 Sv from the West Pacific warm pool to … See more
The Atlantic NECC consists of the eastward zonal transport of water between 3°N and 9°N, with typical widths on the order of 300 km. The Atlantic NECC is unique among the … See more
The Pacific NECC is known to be stronger during classic El Niño events, when there is an anomalous warming of the eastern and central Pacific … See more
Wikipedia text under CC-BY-SA license Equatorial Counter Current - Oxford Reference
WEBLearn how trade winds drive both North and South Equatorial Currents westward, and how Equatorial Counter Currents and Under Currents return some warm waters eastward. Explore the Intertropical Convergence …
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What explains the eastward flow of the equatorial counter-current?
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Highly variable deep-sea currents over tidal and seasonal
Department Press Briefing – July 24, 2024