Articles | Volume 17, issue 23
https://doi.org/10.5194/bg-17-6051-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-6051-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Reviews and syntheses: Present, past, and future of the oxygen minimum zone in the northern Indian Ocean
Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstr. 6, 28359
Bremen, Germany
Greg Cowie
School of Geosciences, University of Edinburgh, James Hutton Road,
Edinburgh EH9 3FE, Scotland, UK
Birgit Gaye
Institute for Geology, Universität Hamburg, Bundesstraße 55, 20146
Hamburg, Germany
Joaquim Goes
Marine Biology, Department of Marine Biology and Paleoenvironment, Lamont–Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades,
New York 10964, USA
Helga do Rosário Gomes
Marine Biology, Department of Marine Biology and Paleoenvironment, Lamont–Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades,
New York 10964, USA
Raleigh R. Hood
Horn Point Laboratory, University of Maryland Center for Environmental
Science, P.O. Box 775, Cambridge, MD 21613, USA
Zouhair Lachkar
Center for Prototype Climate Modeling (CPCM), NYU, Abu Dhabi, UAE
Henrike Schmidt
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Duesternbrooker Weg 20,
24105 Kiel, Germany
Joachim Segschneider
Institute of Geosciences, Christian-Albrechts-Universität zu Kiel (CAU),
Ludewig-Meyn-Straße 10, 24118 Kiel, Germany
Arvind Singh
Geosciences Division, Physical Research Laboratory (PRL) Navrangpura,
Ahmedabad 380 009, India
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Latest update: 13 Dec 2024
Short summary
The northern Indian Ocean hosts an extensive oxygen minimum zone (OMZ), which intensified due to human-induced global changes. This includes the occurrence of anoxic events on the Indian shelf and affects benthic ecosystems and the pelagic ecosystem structure in the Arabian Sea. Consequences for biogeochemical cycles are unknown, which, in addition to the poor representation of mesoscale features, reduces the reliability of predictions of the future OMZ development in the northern Indian Ocean.
The northern Indian Ocean hosts an extensive oxygen minimum zone (OMZ), which intensified due to...
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