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The Pacific NECC is a major eastward moving surface current that transports more than 20 Sv from the West Pacific warm pool to the cooler east Pacific. In the western Pacific the countercurrent is centred near 5°N while in the central Pacific it is located near 7°N.

The Pacific Equatorial Countercurrent is very strong and is definable year-round. The Atlantic Equatorial Countercurrent is strongest off the coast of Ghana (Africa), where it is known as the Guinea Current. The countercurrent of the Indian Ocean flows only during the northern winter and only south… Read More; Pacific North Equatorial Current

Equatorial countercurrent, current phenomenon noted near the equator, an eastward flow of oceanic water in opposition to and flanked by the westward equatorial currents of the Atlantic, Pacific, and Indian oceans.

Jul 16, 2020 · The North Equatorial Subsurface Current (NESC) has recently been found to flow westward below the North Equatorial Countercurrent in the subsurface layer across the Pacific Ocean.

Apr 14, 2023 · Like the name implies, these currents run counter to the prevailing wind direction but usually only in regions where the winds are weak. These currents are located along the equator and are a result of the water returning east after it …

Jun 1, 2021 · The structure and variations of the North Equatorial Countercurrent (NECC) in the far western Pacific Ocean during 2014–16 are investigated using repeated in situ hydrographic data, altimeter data, Argo data, and reanalysis data.

Apr 15, 2013 · Two patches of large-magnitude wind stress curl are noticeable in the tropical North Pacific. The western patch locates in the off-equatorial western Pacific (150°–170°E, 5°–15°N). The eastern patch is centered at around 5°N and exists in the entire central-to-eastern Pacific basin (180°–130°W).

Located at the crossroads of the tropical and subtropical circulations, the westward-flowing North Equatorial Current (NEC) and its subsequent bifurcation off the Philippine coast near 13°N serve as important pathways for heat and water mass exchanges between the mid- and low-latitude North Pacific Ocean.

A comprehensive physical and dynamical picture of the Pacific Equatorial Countercurrent is presented. This is the first known attempt; to analyze an ocean current system on the basis of the totality of hydrographic and wind stress data available.

Jun 1, 2012 · [2] The North Equatorial Countercurrent (NECC), flowing eastward across the tropical Pacific Ocean between 2°N and 10°N, can be regarded as a boundary between the North and South Pacific tropical gyres [Wyrtki and Kendall, 1967; Philander et al., 1987; Reverdin et al., 1994; Donguy and Meyers, 1996].