Deoxygenation in the oxygen minimum zone of the eastern tropical North Atlantic.
Open accessAbstract
Observations and model results both indicate increasing oxygen minimum zones (OMZ) in the tropical oceans. Here we report on record low dissolved oxygen minimum concentrations in the eastern tropical North Atlantic in fall of 2008, with less than 40 μ mol kg−1 in the core of the OMZ. There we find a deoxygenation rate of ∼0.5 μ mol kg−1 a−1 during the last decades on two repeat sections at 7.5 and 11°N. The potential temperature and salinity in the surface and central water layers increased on both sections compared to previous observations. However, in contrast to the oxygen decrease in the core of the OMZ, increasing oxygen concentrations were observed in the central water layer above the OMZ. The observed deoxygenation was thus restricted to the core of the oxygen minimum layer. It remains unclear whether the vertical expansion of the oxygen minimum represents a long time trend or decadal variations.
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Based on oxygen observations from repeat ship sections in the OMZ of the eastern tropical North Atlantic for the recent decade (2006-2015), Hahn et al. (2017) suggested the existence of strong oxygen variations over this decade superimposed on the multi-decadal deoxygenation pattern.
“Based on oxygen observations from repeat ship sections in the OMZ of the eastern tropical North Atlantic for the recent decade (2006)(2007)(2008)(2009)(2010)(2011)(2012)(2013)(2014)(2015), Hahn et al. (2017) suggested the existence of strong oxygen variations over this decade that are superimposed on the multi-decadal deoxygenation pattern (Stramma et al., 2009;Brandt et al., 2015;Santos et al., 2”
From The tropical atlantic observing system (2019) · cites this paper as Stramma et al., 2009
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Oxygen minimum zones in the eastern tropical Atlantic and Pacific oceans
Karstensen, J., Stramma, L., & Visbeck, M. (2008) · Progress in Oceanography · doi:10.1016/j.pocean.2007.05.009 · Cited by 666 · see citing works
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- Arhan, M., H. Mercier, B. Bourles, and Y. Gouriou (1998), Hydrographic section across the Atlantic at 7°30 0 N and 4°30 0 S, Deep Sea Res., Part I, 45, 829 -872, doi:10.1016/S0967-0637(98)00001-6. · DOI
- Bopp, L., C. Le Quere, M. Heimann, A. C. Manning, and P. Monfray (2002), Climate induced oceanic oxygen fluxes: Implications for the contemporary carbon budget, Global Biogeochem. Cycles, 16(2), 1022, doi:10.1029/2001GB001445. · DOI
- Curry, R., B. Dickson, and I. Yashayaev (2003), A change in the freshwater balance of the Atlantic Ocean over the past four decades, Nature, 426, 826 -829, doi:10.1038/nature02206. · DOI
- Gouretski, V. V., and K. Jancke (2000), Systematic errors as the cause for an apparent deep water property variability: Global analysis of the WOCE and historical hydrographic data, Prog. Oceanogr., 48, 337 -402, doi:10.1016/S0079-6611(00)00049-5. · DOI
- Hofmann, M., and H.-J. Schellnhuber (2009), Oceanic acidification affects marine carbon pump and triggers extended marine oxygen holes, Proc. Natl. Acad. Sci. U. S. A., 106, 3017 -3022, doi:10.1073/pnas. 0813384106. · DOI
- Keeling, R. F., and H. E. Garcia (2002), The change in oceanic O 2 inven- tory associated with recent global warming, Proc. Natl. Acad. Sci. U. S. A., 99, 7848 -7853, doi:10.1073/pnas.122154899. · DOI · Paper page
- Levitus, S., J. I. Antonov, T. P. Boyer, and C. Stephens (2000), Warming of the world ocean, Science, 287, 2225 -2229, doi:10.1126/ science.287.5461.2225. · DOI
- Matear, R. J., and C. Hirst (2003), Long-term changes in dissolved oxygen concentrations in the ocean caused by protracted global warming, Global Biogeochem. Cycles, 17(4), 1125, doi:10.1029/2002GB001997. · DOI
- Oschlies, A., K. G. Schulz, U. Riebesell, and A. Schmittner (2008), Simu- lated 21st century's increase in oceanic suboxia by CO 2 -enhanced biotic carbon export, Global Biogeochem. Cycles, 22, GB4008, doi:10.1029/ 2007GB003147. · DOI
- Prince, E. D., and C. P. Goodyear (2006), Hypoxia-based habitat compres- sion of tropical pelagic fishes, Fish. Oceanogr., 15, 451 -464, doi:10.1111/j.1365-2419.2005.00393.x. · DOI
- Siedler, G., N. Zangenberg, R. Onken, and A. Morliere (1992), Seasonal changes in the tropical Atlantic circulation observations and simulations of the Guinea Dome, J. Geophys. Res., 97, 703 -715, doi:10.1029/ 91JC02501. · DOI · Paper page
- Stramma, L., P. Brandt, J. Schafstall, F. Schott, J. Fischer, and A. Ko ¨rtzinger (2008a), Oxygen minimum zone in the eastern North Atlantic south and east of the Cape Verde Islands, J. Geophys. Res., 113, C04014, doi:10.1029/2007JC004369. · DOI
- Stramma, L., G. C. Johnson, J. Sprintall, and V. Mohrholz (2008b), Expanding oxygen-minimum zones in the tropical oceans, Science, 320, 655 -658, doi:10.1126/science.1153847. · DOI
- Vaquer-Sunyer, R., and C. M. Duarte (2008), Thresholds of hypoxia for marine biodiversity, Proc. Natl. Acad. Sci. U. S. A., 105, 15,452 -15,457, doi:10.1073/pnas.0803833105. · DOI · Paper page
- Wallace, D. W. R., and H. W. Bange (2004), Introduction to special section: Results of the Meteor 55: Tropical SOLAS Expedition, Geophys. Res. Lett., 31, L23S01, doi:10.1029/2004GL021014. · DOI
- Whitney, F. A., H. J. Freeland, and M. Robert (2007), Persistently declining oxygen levels in the interior waters of the eastern subarctic Pacific, Prog. Oceanogr., 75, 179 -199, doi:10.1016/j.pocean.2007.08.007. · DOI
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Brandt, P., Bange, H. W., Banyte, D., Dengler, M., Didwischus, S.-H., Fischer, T., Greatbatch, R. J., Hahn, J., Kanzow, T., Karstensen, J., et al. (2015) · Biogeosciences · doi:10.5194/bg-12-489-2015 · Cited by 180 · see citing works
Self-citationThe tropical atlantic observing system
Foltz, G. R., Brandt, P., Richter, I., Rodríguez-Fonseca, B., Hernandez, F., Dengler, M., Rodrigues, R. R., Schmidt, J. O., Yu, L., Lefevre, N., et al. (2019) · Frontiers in Marine Science · doi:10.3389/fmars.2019.00206 · Cited by 150 · see citing works
Self-citationOcean scale hypoxia-based habitat compression of Atlantic istiophorid billfishes
PRINCE, E. D., LUO, J., PHILLIP GOODYEAR, C., HOOLIHAN, J. P., SNODGRASS, D., ORBESEN, E. S., SERAFY, J. E., ORTIZ, M., & SCHIRRIPA, M. J. (2010) · Fisheries Oceanography · doi:10.1111/j.1365-2419.2010.00556.x · Cited by 140 · see citing works
Open ocean dead zones in the tropical North Atlantic Ocean.
Karstensen, J., Fiedler, B., Schütte, F., Brandt, P., Körtzinger, A., Fischer, G., Zantopp, R., Hahn, J., Visbeck, M., & Wallace, D. (2015) · Biogeosciences · doi:10.5194/bg-12-2597-2015 · Cited by 105 · see citing works
Self-citationHahn, J., Brandt, P., Greatbatch, R. J., Krahmann, G., & Körtzinger, A. (2014) · Climate Dynamics · doi:10.1007/s00382-014-2065-0 · Cited by 48 · see citing works
Self-citation
- Authors
- Stramma, L., Visbeck, M., Brandt, P., Tanhua, T., & Wallace, D.
- Affiliations
- Christian-Albrechts-Universität zu Kiel (DE)
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2009-10
- Volume
- 36
- Issue
- 20
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2052367381
- Cited by
- 52
- References
- 1
- Citations by year
- 2026: 1 · 2024: 2 · 2023: 5 · 2022: 2 · 2021: 1 · 2020: 1 · 2019: 3 · 2018: 1 · 2017: 4 · 2016: 10 · 2015: 5 · 2014: 2 · 2013: 4 · 2012: 6
- FWCI
- 2.56
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Geophysical Research Letters (publishedVersion)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion, other-oa)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Biology and Ecology Research
- Keywords
- oxygen minimum zone, ocean deoxygenation, eastern tropical North Atlantic, dissolved oxygen, Central Water, surface water warming, decadal variability
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