Research Institute for Global Change, Japan Agency for Marine-Earth
Science and Technology (JAMSTEC), 3173-25, Showa-machi, Kanazawa-ku,
Yokohama, Kanagawa, 236-0001, Japan
Research Institute for Global Change, Japan Agency for Marine-Earth
Science and Technology (JAMSTEC), 3173-25, Showa-machi, Kanazawa-ku,
Yokohama, Kanagawa, 236-0001, Japan
Research Institute for Global Change, Japan Agency for Marine-Earth
Science and Technology (JAMSTEC), 3173-25, Showa-machi, Kanazawa-ku,
Yokohama, Kanagawa, 236-0001, Japan
Tomohiro Hajima
Research Institute for Global Change, Japan Agency for Marine-Earth
Science and Technology (JAMSTEC), 3173-25, Showa-machi, Kanazawa-ku,
Yokohama, Kanagawa, 236-0001, Japan
Masahiro Watanabe
Atmosphere and Ocean Research Institute, the University of Tokyo,
5-1-5, Kashiwanoha, Kashiwa, Chiba, 277-8564, Japan
Michio Kawamiya
Research Institute for Global Change, Japan Agency for Marine-Earth
Science and Technology (JAMSTEC), 3173-25, Showa-machi, Kanazawa-ku,
Yokohama, Kanagawa, 236-0001, Japan
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Total article views: 2,665 (including HTML, PDF, and XML)
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2,029
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2,665
223
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148
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PDF: 539
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Supplement: 223
BibTeX: 117
EndNote: 148
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436
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Total article views: 3,460 (including HTML, PDF, and XML)
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Total article views: 2,665 (including HTML, PDF, and XML)
Thereof 2,524 with geography defined
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Total article views: 795 (including HTML, PDF, and XML)
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Carbon flux between air and sea is known to fluctuate in response to inherent climate variations. In this study, observed ocean hydrographic data were assimilated into Earth system models, and the carbon flux in the equatorial Pacific was evaluated. Our results suggest that, when observed ocean hydrographic data are assimilated into models for carbon cycle predictions on interannual to decadal timescales, the reproducibility of the internal climate variations in the model itself is important.
Carbon flux between air and sea is known to fluctuate in response to inherent climate...
