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First oceanographic survey of the entire continental shelf adjacent to the northern Agulhas Current ArchiMer
Lutjeharms, Johann; Durgadoo, Jonathan V.; Schapira, Mathilde; Mcquaid, Christopher D..
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Ano: 2010 URL: https://archimer.ifremer.fr/doc/00174/28534/26917.pdf
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Upper-layer circulation in the eastern Equatorial and South Atlantic Ocean in January-March 1995 ArchiMer
Mercier, Herle; Arhan, Michel; Lutjeharms, Johann.
The upper-layer circulation in the eastern basin of the South Atlantic was studied from hydrographic and direct velocity measurements along WOCE lines A11, A13 and A14. A13 and A14 provide quasi-meridional samplings of the equatorial, subequatorial and subtropical circulation regimes. A13 was carried out along the African coast at about 600 km offshore from it, and A 14 along the nominal longitude 9degreesW. A11 intersects the Cape Basin between 46degreesS in the west and 30degreesS in the east. Transport estimates were derived from direct velocity measurements and a box inverse model. In the equatorial eastern Atlantic, the Equatorial Undercurrent (EUC) transport decreases from 25x10(6) m(3) s(-1) at 9degreesW to 13x10(6) m(3) s(-1) at 5degreesE....
Tipo: Text Palavras-chave: Hydrography; Current; Circulation; South Atlantic; Equatorial Atlantic.
Ano: 2003 URL: https://archimer.ifremer.fr/doc/2003/publication-460.pdf
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An altimetry-based gravest empirical mode south of Africa: 1. Development and validation ArchiMer
Swart, Sebastiaan; Speich, Sabrina; Ansorge, Isabelle J.; Lutjeharms, Johann.
Hydrographic transects of the Antarctic Circumpolar Current (ACC) south of Africa are projected into baroclinic stream function space parameterized by pressure and dynamic height. This produces a two-dimensional gravest empirical mode (GEM) that captures more than 97% of the total density and temperature variance in the ACC domain. Weekly maps of absolute dynamic topography data, derived from satellite altimetry, are combined with the GEM to obtain a 16 year time series of temperature and salinity fields. The time series of thermohaline fields are compared with independent in situ observations. The residuals decrease sharply below the thermocline and through the entire water column the mean root-mean-square (RMS) error is 0.15 degrees C, 0.02, and 0.02 kg...
Tipo: Text
Ano: 2010 URL: http://archimer.ifremer.fr/doc/00008/11901/8613.pdf
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