Publications des scientifiques de l'IRD

Ibanhez J. S. P., Diverrès Denis, Araujo M., Lefèvre Nathalie. (2015). Seasonal and interannual variability of sea-air CO2 fluxes in the tropical Atlantic affected by the Amazon River plume. Global Biogeochemical Cycles, 29 (10), p. 1640-1655. ISSN 0886-6236.

Titre du document
Seasonal and interannual variability of sea-air CO2 fluxes in the tropical Atlantic affected by the Amazon River plume
Année de publication
2015
Type de document
Article référencé dans le Web of Science WOS:000364876500005
Auteurs
Ibanhez J. S. P., Diverrès Denis, Araujo M., Lefèvre Nathalie
Source
Global Biogeochemical Cycles, 2015, 29 (10), p. 1640-1655 ISSN 0886-6236
CO2 fugacities obtained from a merchant ship sailing from France to French Guyana were used to explore the seasonal and interannual variability of the sea-air CO2 exchange in the western tropical North Atlantic (TNA; 5-14 degrees N, 41-52 degrees W). Two distinct oceanic water masses were identified in the area associated to the main surface currents, i.e., the North Brazil Current (NBC) and the North Equatorial Current (NEC). The NBC was characterized by permanent CO2 oversaturation throughout the studied period, contrasting with the seasonal pattern identified in the NEC. The NBC retroflection was the main contributor to the North Equatorial Counter Current (NECC), thus spreading into the central TNA, the Amazon River plume, and the CO2-rich waters probably originated from the equatorial upwelling. Strong CO2 undersaturation was associated to the Amazon River plume. Total inorganic carbon drawdown due to biological activity was estimated to be 154 mu mol kg(-1) within the river plume. As a consequence, the studied area acted as a net sink of atmospheric CO2 (from -72.2 +/- 10.2 mmol m(-2) month(-1) in February to 14.3 +/- 4.5 mmol m(-2) month(-1) in May). This contrasted with the net CO2 efflux estimated by the main global sea-air CO2 flux climatologies. Interannual sea surface temperature changes in the TNA caused by large-scale climatic events could determine the direction and intensity of the sea-air CO2 fluxes in the NEC. Positive temperature anomalies observed in the TNA led to an almost permanent CO2 outgassing in the NEC in 2010.
Plan de classement
Limnologie physique / Océanographie physique [032]
Description Géographique
ATLANTIQUE ; AMAZONE ; ZONE TROPICALE
Localisation
Fonds IRD [F B010065457]
Identifiant IRD
fdi:010065457
Contact