Lefèvre Nathalie auteur aut IRD Tyaquica P. auteur aut IRD Veleda D. auteur aut IRD Perruche C. auteur aut IRD van Gennip S. J. auteur aut IRD text journalArticle eng text/pdf reformatted digital access The surface fugacity of CO2 (fCO(2)) has been measured hourly at a mooring at 8 degrees N, 38 degrees W, using a spectrophotometric CO2 sensor, from June to October 2013. In September 2013, the fCO(2) and the sea surface salinity (SSS) decrease significantly. The high precipitation due to the presence of the Intertropical Convergence Zone (ITCZ) and the propagation of low salinity waters from the Amazon River plume explain the decrease of SSS. Indeed, in fall, the retroflection of the North Brazil Current (NBC) feeds the North Equatorial Counter Current (NECC) and transports Amazon waters to the eastern part of the tropical Atlantic. Simulations from a three dimensional physical and biogeochemical model and observations at the mooring show that the Amazon plume reached the mooring in September 2013. The decrease of fCO(2) is associated with a moderate peak of chlorophyll. Over the period of the CO2 observations, the site is a source of CO2 to the atmosphere of 0.65 +/- 0.47 mmol m(-2) day(-1). Although the wind speed is at its lowest intensity in September 2013, the flux over the whole period would be about 14% higher without this month. Every month of September from 2006 to 2017, the model simulates a decrease of dissolved inorganic carbon corresponding to the SSS minimum. specialized Fugacity of CO2 Air-sea flux of CO2 Western tropical Atlantic Amazon plume AMAZONE ATLANTIQUE BRESIL 032 211 103419 [11 p.] 2020 0924-7963 https://www.documentation.ird.fr/hor/fdi:010079555 10.1016/j.jmarsys.2020.103419 0924-7963 [F B010079555] https://www.documentation.ird.fr/hor/fdi:010079555 https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers20-09/010079555.pdf IRD - Base Horizon / Pleins textes 2020-10-09 2025-02-24 fdi:010079555 fre