Transports and budgets of anthropogenic CO2 in the tropical North Atlantic in 1992-1993 and 2010-2011

• Published in: Global Biogeochemical Cycles
• Main Authors: Zunino, Patricia, Pérez, Fiz F., Fajar, Noelia M., Guallart, Elisa F., Ríos, Aida F., Pelegrí Llopart,José Luis, Hernández-Guerra, Alonso
• Other Authors: Hernandez-Guerra, Alonso, Fernandez Perez, Fiz, Pelegri, Josep L., Fajar, Noelia, 26647237400, 56598611300, 55246485900, 56180059300, 7103240290, 7003869003, 56455072400, 2600239, 145213, 3902456, 4783466, 329342, 358123, 660191
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2015
• Subjects: 251007 Oceanografía física; Anthropogenic CO2; Transport; Storage rate; Air‐sea fluxes; Changes in circulation; Tropical North Atlantic; North Atlantic Deep Water; North Atlantic
• Online Access: http://hdl.handle.net/10553/52756; https://doi.org/10.1002/2014GB005075

The meridional transport of anthropogenic CO2 (Cant) in the tropical North Atlantic (TNA) is investigated using data from transoceanic sections along 7.5°N and 24.5°N, carried out in the early 1990s and 2010s. The net Cant transport across both sections is northward. At 7.5°N, this transport increased from 315 ± 47 kmol s−1 in 1993 to 493 ± 51 kmol s−1 in 2010; similarly, across 24.5°N it grew from 530 ± 46 kmol s−1 in 1992 to 662 ± 49 kmol s−1 in 2011. These changes result from modifications in the intermediate and deep circulation patterns, as well as from Cant increase within the thermocline waters. In deep waters, lateral advection causes a net Cant input of 112 ± 60 kmol s−1 (234 ± 65 kmol s−1) in 1992–1993 (2010–2011); within these deep waters, the storage rate of Cant is not statistically different from the net Cant input, 139 ± 21 kmol s−1 (188 ± 21 kmol s−1) in 1992–1993 (2010–2011). The Cant increase in deep waters is due to the large injection of Cant across the 24.5°N by the Deep Western Boundary Current and the northward recirculation of North Atlantic Deep Water along 7.5°N. In contrast, a large net Cant output in the upper layer is caused by the Florida Current. Despite this net Cant output, the Cant accumulates at a rate of 215 ± 24 kmol s−1 (291 ± 24 kmol s−1) referenced to year 1993 (2010). From the two Cant budgets, we infer a Cant air‐sea flux of 0.23 ± 0.02 Pg yr−1in the TNA, much larger than previous estimates.