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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- Oxygen minimum zone along the eastern Arabian Sea: Intra-annual variation and dynamics based on ship-borne studies V. Sudheesh et al. 10.1016/j.pocean.2022.102742
- Deoxygenation in Marginal Seas of the Indian Ocean S. Naqvi 10.3389/fmars.2021.624322
- Causes of uncertainties in the representation of the Arabian Sea oxygen minimum zone in CMIP5 models H. Schmidt et al. 10.5194/os-17-1303-2021
- A Regional Review of Marine and Coastal Impacts of Climate Change on the ROPME Sea Area S. Lincoln et al. 10.3390/su132413810
- Organic Matter Supply and Utilization in Oxygen Minimum Zones A. Engel et al. 10.1146/annurev-marine-041921-090849
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- Oxygen and Nutrient Trapping in the Southern Benguela Upwelling System T. Rixen et al. 10.3389/fmars.2021.730591
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- Mapping manifestations of parametric uncertainty in projected pelagic oxygen concentrations back to contemporary local model fidelity U. Löptien et al. 10.1038/s41598-021-00334-2
- Influence of warm core eddy on the vertical distribution of autotrophic pico- and nanoplankton in the Bay of Bengal A. Mohan & A. Biju 10.1080/17451000.2021.1872795
- Determining the Distribution of Fluorescent Organic Matter in the Indian Ocean Using in situ Fluorometry M. Shigemitsu et al. 10.3389/fmicb.2020.589262
- Potential role of priming effect in the open ocean oxygen minimum zones: an outlook P. Ragavan & S. Kumar 10.1007/s10750-021-04574-1
12 citations as recorded by crossref.
- Particulate organic matter dynamics and its isotopic signatures (δ13CPOC and δ15NPN) in relation to physical forcing in the central Arabian Sea during SW monsoon (2017–2018) S. Silori et al. 10.1016/j.scitotenv.2021.147326
- Reviews and syntheses: Trends in primary production in the Bay of Bengal – is it at a tipping point? C. Löscher 10.5194/bg-18-4953-2021
- Oxygen minimum zone along the eastern Arabian Sea: Intra-annual variation and dynamics based on ship-borne studies V. Sudheesh et al. 10.1016/j.pocean.2022.102742
- Deoxygenation in Marginal Seas of the Indian Ocean S. Naqvi 10.3389/fmars.2021.624322
- Causes of uncertainties in the representation of the Arabian Sea oxygen minimum zone in CMIP5 models H. Schmidt et al. 10.5194/os-17-1303-2021
- A Regional Review of Marine and Coastal Impacts of Climate Change on the ROPME Sea Area S. Lincoln et al. 10.3390/su132413810
- Organic Matter Supply and Utilization in Oxygen Minimum Zones A. Engel et al. 10.1146/annurev-marine-041921-090849
- Observed variability of monsoon blooms in the north-central Arabian Sea and its implication on oxygen concentration: A bio-argo study T. Mathew et al. 10.1016/j.dsr2.2021.104935
- Oxygen and Nutrient Trapping in the Southern Benguela Upwelling System T. Rixen et al. 10.3389/fmars.2021.730591
- Progress in understanding of Indian Ocean circulation, variability, air–sea exchange, and impacts on biogeochemistry H. Phillips et al. 10.5194/os-17-1677-2021
- Ideas and perspectives: Ushering the Indian Ocean into the UN Decade of Ocean Science for Sustainable Development (UNDOSSD) through marine ecosystem research and operational services – an early career's take K. Nimit 10.5194/bg-18-3631-2021
- Mapping manifestations of parametric uncertainty in projected pelagic oxygen concentrations back to contemporary local model fidelity U. Löptien et al. 10.1038/s41598-021-00334-2
3 citations as recorded by crossref.
- Influence of warm core eddy on the vertical distribution of autotrophic pico- and nanoplankton in the Bay of Bengal A. Mohan & A. Biju 10.1080/17451000.2021.1872795
- Determining the Distribution of Fluorescent Organic Matter in the Indian Ocean Using in situ Fluorometry M. Shigemitsu et al. 10.3389/fmicb.2020.589262
- Potential role of priming effect in the open ocean oxygen minimum zones: an outlook P. Ragavan & S. Kumar 10.1007/s10750-021-04574-1
Latest update: 04 Jun 2023
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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