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• W1815030837 startingPage "n/a" @default.
• W1815030837 abstract "[1] We present results from the first zonal transect of iron, aluminum, and manganese conducted from the western source region of the Equatorial Undercurrent (EUC) to the central equatorial Pacific. Trace metals were elevated along the slope of Papua New Guinea and within the New Guinea Coastal Undercurrent (NGCU), which is the primary Southern Hemisphere entry path of water to the EUC. Subsurface maxima in total acid-soluble iron, aluminum, and manganese were evident in the EUC. These maxima were generally greatest in the western equatorial Pacific and decreased in magnitude eastward. Maxima in iron and aluminum persisted to 140°W; maxima in manganese extended to 175°W. Iron and manganese maxima were deeper (25–75 m) than aluminum maxima and located in the lower EUC, which undergoes less interior ocean mixing than shallower waters. The depth of the aluminum subsurface maxima correlated strongly (r = 0.88) with the depth of the EUC velocity maximum. Surface waters were enriched in aluminum and manganese offshore of Papua New Guinea. Surface metal concentrations decreased eastward throughout the western warm pool up to the longitude (∼180°W) of the salinity front. Detrital sediment input from either direct riverine input or sediment resuspension appeared to be the primary mechanism of supplying metals to the NGCU. We estimated eastward fluxes of metals in the EUC and found greatest fluxes in the western equatorial Pacific between 160°E and 165°E, except for aluminum. Fluxes of aluminum and, to a lesser extent, manganese increased concurrently with water volume transport in the central equatorial Pacific. Iron transport in the EUC remained constant east of the dateline, apparently due to the combined effects of dilution by meridional entrainment and scavenging. Iron was mobilized in a highly active western boundary current region and transported eastward in the lower EUC." @default.
• W1815030837 created "2016-06-24" @default.
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• W1815030837 date "2010-09-01" @default.
• W1815030837 modified "2023-10-18" @default.
• W1815030837 title "Western Pacific coastal sources of iron, manganese, and aluminum to the Equatorial Undercurrent" @default.
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• W1815030837 cites W1634089551 @default.
• W1815030837 cites W1686306396 @default.
• W1815030837 cites W1807406143 @default.
• W1815030837 cites W1884540967 @default.
• W1815030837 cites W1931182741 @default.
• W1815030837 cites W1971010350 @default.
• W1815030837 cites W1974849759 @default.
• W1815030837 cites W1976111679 @default.
• W1815030837 cites W1976278501 @default.
• W1815030837 cites W1976335483 @default.
• W1815030837 cites W1977541820 @default.
• W1815030837 cites W1980773918 @default.
• W1815030837 cites W1985520778 @default.
• W1815030837 cites W1988826310 @default.
• W1815030837 cites W1991705347 @default.
• W1815030837 cites W1993196150 @default.
• W1815030837 cites W1994975574 @default.
• W1815030837 cites W2000478837 @default.
• W1815030837 cites W2002454017 @default.
• W1815030837 cites W2002565545 @default.
• W1815030837 cites W2003618351 @default.
• W1815030837 cites W2004799499 @default.
• W1815030837 cites W2012070200 @default.
• W1815030837 cites W2013298821 @default.
• W1815030837 cites W2013900698 @default.
• W1815030837 cites W2016346783 @default.
• W1815030837 cites W2019476144 @default.
• W1815030837 cites W2022626025 @default.
• W1815030837 cites W2029815620 @default.
• W1815030837 cites W2030784517 @default.
• W1815030837 cites W2036279401 @default.
• W1815030837 cites W2036907212 @default.
• W1815030837 cites W2037332161 @default.
• W1815030837 cites W2039781035 @default.
• W1815030837 cites W2040235417 @default.
• W1815030837 cites W2042936371 @default.
• W1815030837 cites W2050658323 @default.
• W1815030837 cites W2053660667 @default.
• W1815030837 cites W2056707930 @default.
• W1815030837 cites W2057487520 @default.
• W1815030837 cites W2058617522 @default.
• W1815030837 cites W2064040135 @default.
• W1815030837 cites W2067376557 @default.
• W1815030837 cites W2067961116 @default.
• W1815030837 cites W2070331874 @default.
• W1815030837 cites W2074535136 @default.
• W1815030837 cites W2076347268 @default.
• W1815030837 cites W2077711976 @default.
• W1815030837 cites W2078517784 @default.
• W1815030837 cites W2080367040 @default.
• W1815030837 cites W2081188003 @default.
• W1815030837 cites W2083115545 @default.
• W1815030837 cites W2084376607 @default.
• W1815030837 cites W2084429208 @default.
• W1815030837 cites W2085165374 @default.
• W1815030837 cites W2090525362 @default.
• W1815030837 cites W2100820351 @default.
• W1815030837 cites W2102749578 @default.
• W1815030837 cites W2102761435 @default.
• W1815030837 cites W2110433503 @default.
• W1815030837 cites W2110677121 @default.
• W1815030837 cites W2111552504 @default.
• W1815030837 cites W2117031434 @default.
• W1815030837 cites W2124814176 @default.
• W1815030837 cites W2144891223 @default.
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• W1815030837 cites W2146892358 @default.
• W1815030837 cites W2148312937 @default.
• W1815030837 cites W2148343249 @default.
• W1815030837 cites W2163402409 @default.
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• W1815030837 cites W2165028864 @default.
• W1815030837 cites W2166329182 @default.
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• W1815030837 doi "https://doi.org/10.1029/2009gb003693" @default.
• W1815030837 hasPublicationYear "2010" @default.
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