From the western boundary currents to the Pacific Equatorial Undercurrent: Modeled pathways and water mass evolutions
| Type | Article | ||||||||
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| Date | 2011-12 | ||||||||
| Language | English | ||||||||
| Author(s) | Grenier Melanie, Cravatte Sophie1, Blanke Bruno2, Menkes Christophe4, Koch-Larrouy Ariane1, Durand Fabien1, Melet Angelique1, 3, Jeandel Catherine1 | ||||||||
| Affiliation(s) | 1 : LEGOS, F-31400 Toulouse, France. 2 : Univ Bretagne, Lab Phys Oceans, CNRS IFREMER IRD UBO, UMR 6523, F-29238 Brest, France. 3 : Univ Grenoble, CNRS, LEGI, UMR 5519, F-38041 Grenoble 9, France. 4 : Univ Paris 06, LOCEAN, UPMC IRD CNRS MNHN, F-75252 Paris 05, France. |
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| Source | Journal Of Geophysical Research-oceans (0148-0227) (Amer Geophysical Union), 2011-12 , Vol. 116 , N. C12044 , P. 16 p. | ||||||||
| DOI | 10.1029/2011JC007477 | ||||||||
| WOS© Times Cited | 59 | ||||||||
| Abstract | The hydrological and geochemical properties of the waters constituting the Pacific Equatorial Undercurrent (EUC) determine the properties of the equatorial cold tongue. Understanding and quantifying the various EUC origins is therefore of prime importance. For this purpose, a high-resolution (1/4 degrees) interannual oceanic simulation was analyzed from the western tropical Pacific boundaries to 140 degrees W, using a Lagrangian framework. Waters from the Low-Latitude Western Boundary Currents (LLWBCs) transiting from Vitiaz Strait (the main contributor), from Solomon Strait, and via the Mindanao Current were identified as the principal sources to the EUC. Waters conveyed by the interior ocean off equator are negligible till 180 E. The LLWBCs' waters represent 87% of the EUC transport at 156 degrees E out of which the New Guinea Coastal Undercurrent (NGCU) is as large as 47%. The EUC meridional distribution suggests that the waters originating from Solomon Strait and Mindanao Current mostly remain in the hemisphere from which they originate. Contrastingly, Vitiaz Strait waters are found in both hemispheres. The vertical EUC distribution shows that the lower layer of the EUC is mainly composed of Vitiaz Strait waters. Finally, the source transport distributions were characterized, at their origin and within the EUC, as a function of density. These distributions showed that waters flowing through Vitiaz Strait at densities higher than those of the EUC (down to sigma(theta) = 27.2 kg m(-3)) undergo a diapycnal mixing and lighten during their journey to join the EUC. This lightening supports the suggestion that the NGCU is a major source for the EUC geochemical enrichment. | ||||||||
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