Impacts of mesoscale eddies in the South China Sea on biogeochemical cycles.

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Title: Impacts of mesoscale eddies in the South China Sea on biogeochemical cycles.
Authors: Guo, Mingxian, Chai, Fei1, Xiu, Peng2 pxiu@scsio.ac.cn, Li, Shiyu3 eeslsy@mail.sysu.edu.cn, Rao, Shivanesh1
Source: Ocean Dynamics. Sep2015, Vol. 65 Issue 9/10, p1335-1352. 18p.
Subjects: Biogeochemical cycles, Mathematical models of oceanography, Mesoscale eddies, Phytoplankton
Geographic Terms: Pacific Ocean, South China Sea
Abstract: Biogeochemical cycles associated with mesoscale eddies in the South China Sea (SCS) were investigated. The study was based on a coupled physical-biogeochemical Pacific Ocean model (Regional Ocean Model System-Carbon, Silicate, and Nitrogen Ecosystem, ROMS-CoSiNE) simulation for the period from 1991 to 2008. A total of 568 mesoscale eddies with lifetime longer than 30 days were used in the analysis. Composite analysis revealed that the cyclonic eddies were associated with abundance of nutrients, phytoplankton, and zooplankton while the anticyclonic eddies depressed biogeochemical cycles, which are generally controlled by the eddy pumping mechanism. In addition, diatoms were dominant in phytoplankton species due to the abundance of silicate. Dipole structures of vertical fluxes with net upward motion in cyclonic eddies and net downward motion in anticyclonic eddies were revealed. During the lifetime of an eddy, the evolutions of physical, biological, and chemical structures were not linearly coupled at the eddy core where plankton grew, and composition of the community depended not only on the physical and chemical processes but also on the adjustments by the predator-prey relationship. [ABSTRACT FROM AUTHOR]
Copyright of Ocean Dynamics is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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DbLabel: Engineering Source
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  Data: Impacts of mesoscale eddies in the South China Sea on biogeochemical cycles.
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  Data: <searchLink fieldCode="AR" term="%22Guo%2C+Mingxian%22">Guo, Mingxian</searchLink><br /><searchLink fieldCode="AR" term="%22Chai%2C+Fei%22">Chai, Fei</searchLink><relatesTo>1</relatesTo><br /><searchLink fieldCode="AR" term="%22Xiu%2C+Peng%22">Xiu, Peng</searchLink><relatesTo>2</relatesTo><i> pxiu@scsio.ac.cn</i><br /><searchLink fieldCode="AR" term="%22Li%2C+Shiyu%22">Li, Shiyu</searchLink><relatesTo>3</relatesTo><i> eeslsy@mail.sysu.edu.cn</i><br /><searchLink fieldCode="AR" term="%22Rao%2C+Shivanesh%22">Rao, Shivanesh</searchLink><relatesTo>1</relatesTo>
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  Data: <searchLink fieldCode="DE" term="%22Biogeochemical+cycles%22">Biogeochemical cycles</searchLink><br /><searchLink fieldCode="DE" term="%22Mathematical+models+of+oceanography%22">Mathematical models of oceanography</searchLink><br /><searchLink fieldCode="DE" term="%22Mesoscale+eddies%22">Mesoscale eddies</searchLink><br /><searchLink fieldCode="DE" term="%22Phytoplankton%22">Phytoplankton</searchLink>
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  Data: <searchLink fieldCode="DE" term="%22Pacific+Ocean%22">Pacific Ocean</searchLink><br /><searchLink fieldCode="DE" term="%22South+China+Sea%22">South China Sea</searchLink>
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  Data: Biogeochemical cycles associated with mesoscale eddies in the South China Sea (SCS) were investigated. The study was based on a coupled physical-biogeochemical Pacific Ocean model (Regional Ocean Model System-Carbon, Silicate, and Nitrogen Ecosystem, ROMS-CoSiNE) simulation for the period from 1991 to 2008. A total of 568 mesoscale eddies with lifetime longer than 30 days were used in the analysis. Composite analysis revealed that the cyclonic eddies were associated with abundance of nutrients, phytoplankton, and zooplankton while the anticyclonic eddies depressed biogeochemical cycles, which are generally controlled by the eddy pumping mechanism. In addition, diatoms were dominant in phytoplankton species due to the abundance of silicate. Dipole structures of vertical fluxes with net upward motion in cyclonic eddies and net downward motion in anticyclonic eddies were revealed. During the lifetime of an eddy, the evolutions of physical, biological, and chemical structures were not linearly coupled at the eddy core where plankton grew, and composition of the community depended not only on the physical and chemical processes but also on the adjustments by the predator-prey relationship. [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Ocean Dynamics is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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        Value: 10.1007/s10236-015-0867-1
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        Text: English
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        StartPage: 1335
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      – SubjectFull: Biogeochemical cycles
        Type: general
      – SubjectFull: Mathematical models of oceanography
        Type: general
      – SubjectFull: Mesoscale eddies
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      – SubjectFull: Phytoplankton
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      – SubjectFull: Pacific Ocean
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      – SubjectFull: South China Sea
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              Text: Sep2015
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