2019
DOI: 10.1016/j.pocean.2018.10.006
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The sea-air CO2 net fluxes in the South Atlantic Ocean and the role played by Agulhas eddies

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Cited by 19 publications
(43 citation statements)
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“…As expected, the pH changes observed in the South Atlantic Ocean for the deep and bottom layers are smaller than all other layers, namely, −0.0010/−0.0000 yr −1 for the upper and lower varieties of CDW, −0.0005/−0.0000 yr −1 for upper and lower varieties of NADW, and −0.0000 yr −1 for AABW e.g., [3,5,6]. Additionally, Orselli et al [34] observed that the Agulhas eddies are capable of removing more CO 2 from the atmosphere than their surrounding waters. This intensification of CO 2 absorption at the sea surface is governed mainly by physical processes when the eddy is located in the Eastern basin of the South Atlantic Ocean.…”
Section: Introductionmentioning
confidence: 90%
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“…As expected, the pH changes observed in the South Atlantic Ocean for the deep and bottom layers are smaller than all other layers, namely, −0.0010/−0.0000 yr −1 for the upper and lower varieties of CDW, −0.0005/−0.0000 yr −1 for upper and lower varieties of NADW, and −0.0000 yr −1 for AABW e.g., [3,5,6]. Additionally, Orselli et al [34] observed that the Agulhas eddies are capable of removing more CO 2 from the atmosphere than their surrounding waters. This intensification of CO 2 absorption at the sea surface is governed mainly by physical processes when the eddy is located in the Eastern basin of the South Atlantic Ocean.…”
Section: Introductionmentioning
confidence: 90%
“…The first leg (TAII_01) was conducted from October 24th to November 25th along 35 • S (from Rio Grande, Brazil, to Cape Town, South Africa) [38], and the second leg (TAII_02) was conducted from December 2nd to December 22nd in a Southwestern-Northeastern section (from Cape Town, South Africa, to Rio de Janeiro, Brazil). The FORSA cruise occurred in 2015 on board the Brazilian Navy RV, NPqHo Vital de Oliveira from June 27th to July 15th in a Southwestern-Northeastern section (from Cape Town, to South Africa to Arraial do Cabo, to Brazil) [34,39]. Along these cruise tracks, hydrographic conductivity-temperature-depth (CTD) stations were sampled: 93 in 2011 during the TAII and 12 in 2015 during the FORSA cruise.…”
Section: Cruises Surveysmentioning
confidence: 99%
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