Articles | Volume 12, issue 5
https://doi.org/10.5194/bg-12-1387-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-1387-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
05 Mar 2015
Research article |
| 05 Mar 2015
Rapid acidification of mode and intermediate waters in the southwestern Atlantic Ocean
L. A. Salt
CORRESPONDING AUTHOR
Royal Netherlands Institute for Sea Research, Landsdiep 4, 1797 SZ, Texel, the Netherlands
now at: CNRS, UMR7144, Equipe Chimie Marine, Station Biologique de Roscoff, Place Georges Teissier, 29680 Roscoff, France
S. M. A. C. van Heuven
Centre for Isotope Research, University of Groningen, Nijenborgh 4, 9747 AG, Groningen, the Netherlands
now at: Alfred Wegner Institute, Climate Sciences Department, Postfach 120161, 27515 Bremerhaven, Germany
M. E. Claus
Department of Ocean Ecosystems, University of Groningen, Nijenborgh 7, 9747 AG, Groningen, the Netherlands
E. M. Jones
Alfred Wegener Institute for Polar and Marine Research, 120161, 27515, Bremerhaven, Germany
H. J. W. de Baar
Royal Netherlands Institute for Sea Research, Landsdiep 4, 1797 SZ, Texel, the Netherlands
Department of Ocean Ecosystems, University of Groningen, Nijenborgh 7, 9747 AG, Groningen, the Netherlands
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Cited
20 citations as recorded by crossref.
- Seawater acidification and anthropogenic carbon distribution on the continental shelf and slope of the western South Atlantic Ocean M. Carvalho-Borges et al. 10.1016/j.jmarsys.2018.06.008
- The Western South Atlantic Ocean in a High-CO2 World: Current Measurement Capabilities and Perspectives R. Kerr et al. 10.1007/s00267-015-0630-x
- Anthropogenic CO2 and ocean acidification in Argentine Basin Water Masses over almost five decades of observations M. Fontela et al. 10.1016/j.scitotenv.2021.146570
- Diagnosing CO2 emission-induced feedbacks between the Southern Ocean carbon cycle and the climate system: A multiple Earth System Model analysis using a water mass tracking approach T. Roy et al. 10.1175/JCLI-D-20-0889.1
- Ocean Acidification and Long‐Term Changes in the Carbonate System Properties of the South Atlantic Ocean A. Piñango et al. 10.1029/2021GB007196
- Influence of Changes in pH and Temperature on the Distribution of Apparent Iron Solubility in the Oceans K. Zhu et al. 10.1029/2022GB007617
- Variability of nutrients and carbon dioxide in the Antarctic Intermediate Water between 1990 and 2014 E. Panassa et al. 10.1007/s10236-018-1131-2
- The Effect of Agulhas Eddies on Absorption and Transport of Anthropogenic Carbon in the South Atlantic Ocean I. Orselli et al. 10.3390/cli7060084
- Long‐Term Trends in Phytoplankton Chlorophyll a and Size Structure in the Benguela Upwelling System T. Lamont et al. 10.1029/2018JC014334
- The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives I. ORSELLI et al. 10.1590/0001-3765202220210825
- Siderophores as an iron source for picocyanobacteria in deep chlorophyll maximum layers of the oligotrophic ocean S. Hogle et al. 10.1038/s41396-022-01215-w
- Ocean Ventilation Controls the Contrasting Anthropogenic CO2 Uptake Rates Between the Western and Eastern South Atlantic Ocean Basins H. Gao et al. 10.1029/2021GB007265
- On the influence of Subtropical Mode Water on the South Atlantic Ocean A. Souza et al. 10.1016/j.jmarsys.2018.04.006
- Decadal acidification in the water masses of the Atlantic Ocean A. Ríos et al. 10.1073/pnas.1504613112
- How fast is the Patagonian shelf-break acidifying? I. Orselli et al. 10.1016/j.jmarsys.2017.10.007
- Source waters contribution to the tropical Atlantic central layer: New insights on the Indo-Atlantic exchanges E. Azar et al. 10.1016/j.dsr.2020.103450
- Diagnosing oceanic nutrient deficiency C. Moore 10.1098/rsta.2015.0290
- Formation and Maintenance of the GEOTRACES Subsurface‐Dissolved Iron Maxima in an Ocean Biogeochemistry Model A. Pham & T. Ito 10.1029/2017GB005852
- The sea-air CO2 net fluxes in the South Atlantic Ocean and the role played by Agulhas eddies I. Orselli et al. 10.1016/j.pocean.2018.10.006
- Sea-air carbon dioxide fluxes along 35°S in the South Atlantic Ocean J. Lencina-Avila et al. 10.1016/j.dsr.2016.06.004
20 citations as recorded by crossref.
- Seawater acidification and anthropogenic carbon distribution on the continental shelf and slope of the western South Atlantic Ocean M. Carvalho-Borges et al. 10.1016/j.jmarsys.2018.06.008
- The Western South Atlantic Ocean in a High-CO2 World: Current Measurement Capabilities and Perspectives R. Kerr et al. 10.1007/s00267-015-0630-x
- Anthropogenic CO2 and ocean acidification in Argentine Basin Water Masses over almost five decades of observations M. Fontela et al. 10.1016/j.scitotenv.2021.146570
- Diagnosing CO2 emission-induced feedbacks between the Southern Ocean carbon cycle and the climate system: A multiple Earth System Model analysis using a water mass tracking approach T. Roy et al. 10.1175/JCLI-D-20-0889.1
- Ocean Acidification and Long‐Term Changes in the Carbonate System Properties of the South Atlantic Ocean A. Piñango et al. 10.1029/2021GB007196
- Influence of Changes in pH and Temperature on the Distribution of Apparent Iron Solubility in the Oceans K. Zhu et al. 10.1029/2022GB007617
- Variability of nutrients and carbon dioxide in the Antarctic Intermediate Water between 1990 and 2014 E. Panassa et al. 10.1007/s10236-018-1131-2
- The Effect of Agulhas Eddies on Absorption and Transport of Anthropogenic Carbon in the South Atlantic Ocean I. Orselli et al. 10.3390/cli7060084
- Long‐Term Trends in Phytoplankton Chlorophyll a and Size Structure in the Benguela Upwelling System T. Lamont et al. 10.1029/2018JC014334
- The marine carbonate system along the northern Antarctic Peninsula: current knowledge and future perspectives I. ORSELLI et al. 10.1590/0001-3765202220210825
- Siderophores as an iron source for picocyanobacteria in deep chlorophyll maximum layers of the oligotrophic ocean S. Hogle et al. 10.1038/s41396-022-01215-w
- Ocean Ventilation Controls the Contrasting Anthropogenic CO2 Uptake Rates Between the Western and Eastern South Atlantic Ocean Basins H. Gao et al. 10.1029/2021GB007265
- On the influence of Subtropical Mode Water on the South Atlantic Ocean A. Souza et al. 10.1016/j.jmarsys.2018.04.006
- Decadal acidification in the water masses of the Atlantic Ocean A. Ríos et al. 10.1073/pnas.1504613112
- How fast is the Patagonian shelf-break acidifying? I. Orselli et al. 10.1016/j.jmarsys.2017.10.007
- Source waters contribution to the tropical Atlantic central layer: New insights on the Indo-Atlantic exchanges E. Azar et al. 10.1016/j.dsr.2020.103450
- Diagnosing oceanic nutrient deficiency C. Moore 10.1098/rsta.2015.0290
- Formation and Maintenance of the GEOTRACES Subsurface‐Dissolved Iron Maxima in an Ocean Biogeochemistry Model A. Pham & T. Ito 10.1029/2017GB005852
- The sea-air CO2 net fluxes in the South Atlantic Ocean and the role played by Agulhas eddies I. Orselli et al. 10.1016/j.pocean.2018.10.006
- Sea-air carbon dioxide fluxes along 35°S in the South Atlantic Ocean J. Lencina-Avila et al. 10.1016/j.dsr.2016.06.004
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Latest update: 23 Nov 2024
Short summary
The increase in anthropogenic atmospheric carbon dioxide is mitigated by uptake by the world ocean, which alters the pH of the water. In the South Atlantic we find the highest rates of acidification relative to increase in anthropogenic carbon (Cant) found in Subantarctic Mode Water and Antarctic Intermediate Water. The moderate rates of increase in Cant combined with low buffering capacities, due to low salinity and alkalinity values, have caused rapid acidification in the Subantarctic Zone.
The increase in anthropogenic atmospheric carbon dioxide is mitigated by uptake by the world...
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