Wintertime process study of the North Brazil Current rings reveals the region as a larger sink for CO2 than expected
Open Access
- 21 June 2022
- journal article
- research article
- Published by Copernicus GmbH in Biogeosciences (online)
- Vol. 19 (12), 2969-2988
- https://doi.org/10.5194/bg-19-2969-2022
Abstract
The key processes driving the air–sea CO2 fluxes in the western tropical Atlantic (WTA) in winter are poorly known. WTA is a highly dynamic oceanic region, expected to have a dominant role in the variability in CO2 air–sea fluxes. In early 2020 (February), this region was the site of a large in situ survey and studied in wider context through satellite measurements. The North Brazil Current (NBC) flows northward along the coast of South America, retroflects close to 8∘ N and pinches off the world's largest eddies, the NBC rings. The rings are formed to the north of the Amazon River mouth when freshwater discharge is still significant in winter (a time period of relatively low run-off). We show that in February 2020, the region (5–16∘ N, 50–59∘ W) is a CO2 sink from the atmosphere to the ocean (−1.7 Tg C per month), a factor of 10 greater than previously estimated. The spatial distribution of CO2 fugacity is strongly influenced by eddies south of 12∘ N. During the campaign, a nutrient-rich freshwater plume from the Amazon River is entrained by a ring from the shelf up to 12∘ N leading to high phytoplankton concentration and significant carbon drawdown (∼20 % of the total sink). In trapping equatorial waters, NBC rings are a small source of CO2. The less variable North Atlantic subtropical water extends from 12∘ N northward and represents ∼60 % of the total sink due to the lower temperature associated with winter cooling and strong winds. Our results, in identifying the key processes influencing the air–sea CO2 flux in the WTA, highlight the role of eddy interactions with the Amazon River plume. It sheds light on how a lack of data impeded a correct assessment of the flux in the past, as well as on the necessity of taking into account features at meso- and small scales.Funding Information
- Centre National d’Etudes Spatiales (6146)
- H2020 European Research Council
This publication has 55 references indexed in Scilit:
- Climatological mean and decadal change in surface ocean pCO2, and net sea–air CO2 flux over the global oceansDeep Sea Research Part II: Topical Studies in Oceanography, 2009
- Recommendations for autonomous underway pCO2 measuring systems and data-reduction routinesDeep Sea Research Part II: Topical Studies in Oceanography, 2009
- Amazon River enhances diazotrophy and carbon sequestration in the tropical North Atlantic OceanProceedings of the National Academy of Sciences of the United States of America, 2008
- A significant CO2 sink in the tropical Atlantic Ocean associated with the Amazon River plumeGeophysical Research Letters, 2003
- Global sea–air CO2 flux based on climatological surface ocean pCO2, and seasonal biological and temperature effectsDeep Sea Research Part II: Topical Studies in Oceanography, 2002
- Velocity structure of North Brazil Current ringsGeophysical Research Letters, 2002
- North Brazil Current Ring Generation and Evolution Observed with SeaWiFS*Journal of Physical Oceanography, 2002
- A census of North Brazil Current Rings observed from TOPEX/POSEIDON altimetry: 1992–1998Geophysical Research Letters, 2001
- North Brazil Current retroflection eddiesJournal of Geophysical Research: Oceans, 1994
- Seasonal variation of CO2 and nutrients in the high‐latitude surface oceans: A comparative studyGlobal Biogeochemical Cycles, 1993