Nitrate supply from deep waters to ocean surface waters at 10 °W in the tropical Atlantic Ocean: insight from three decades of monitoring

Kanga Désiré
KOUAME
Centre de Recherches Océanologiques (CRO) 29 Rue des Pêcheurs Treichville BPV 18 Abidjan, Côte d’Ivoire; Université Felix Houphouët-Boigny Laboratoire de Chimie Physique, UFR SSMT, 22 BP 582 Abidjan 22, Côte d’Ivoire Tel: (+225) 0708003608
Aka Marcel KOUASSI, Centre de Recherches Océanologiques (CRO), 29, Rue des Pêcheurs, Treichville BP V 18 Abidjan, Côte d’Ivoire
Albert TROKOUREY, Université Félix Houphouët Boigny (UFHB), Abidjan-Cocody, 01 BV 34 Abidjan 01, Côte d’Ivoire
Kouadio Benjamin N'guessan, Centre de Recherches Océanologiques (CRO), 29, Rue des Pêcheurs, Treichville BP V 18 Abidjan, Côte d’Ivoire, Université Félix Houphouët Boigny (UFHB), Abidjan-Cocody, 01 BV 34 Abidjan 01, Côte d’Ivoire
Marek OSTROWSKI, Institute of Marine Research (IMR) Nordnesgaten 50 Bergen, Norway
Patrice Brehmer, Institut de Recherches pour le Développement IRD, Univ Brest, CNRS, Ifremer, UMR Lemar, Dakar, Senegal
Poster
Mean depth of mixed layer (MLD), nitrate concentrations and nitracline were analyzed at 10 °W to study the seasonal surface supply of nitrate in the tropical Atlantic between 2 °N and 10 °S. Combination of historical and recent data from CTD temperature, salinity and nitrate profiles collected during more three decades (between 1973 and 2007) in the tropical Atlantic Ocean was used to perform this study. The results reveal that in the equatorial zone despite relatively low MLDs in the cold season, a shallow mixing layer (10 > MLD > 30 m) was observed between the equator and 2 °S with average contents of 2. 06 mmol m-3 relatively high nitrate. In contrast to the 0-2 °S area, north of the equator (0-2 °N) while MLDs become shallower, nitrate concentrations decrease to very low concentration (near zero) at 2 °N in the mixed layer (ML). During the warm season, a supply of nitrates associated with deep ML are observed in the equatorial area. Along with such nitrate availability in the sea surface layer, high nitracline is reported both in the ML and below the ML. Meanwhile, nitrate concentrations are very high with a maximum of 7.8 mmol m-3 in the ML at 1 ° N and 1 ° S around 8 m depth. In areas south of the equator despite the observed deepening of the ML, low nitrate concentrations are observed with a nitracline that does not reach the ML. However, at 6 °S an increase in nitrate content (0.67 mmol m-3) followed by a sharp increase between 8 and 8.5 °S (5 mmol m-3) is noted.

Keywords: Equatorial zone; nitracline; area south of the equator; Mixing layer.
Poster PDF