| Project/Area Number |
13440139
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Meteorology/Physical oceanography/Hydrology
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| Research Institution | The University of Tokyo |
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Principal Investigator |
YASUDA Ichiro The University of Tokyo, Graduate School of Science, Associate Professor, 大学院・理学系研究科, 助教授 (80270792)
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| Co-Investigator(Kenkyū-buntansha) |
WATANABE Tomowo Fisheries Research Agency, Marine Productivity Division, Head of the Laboratory, 中央水産研究所・海洋生産部, 室長(研究職)
HIBIYA Toshiyuki The University of Tokyo, Graduate School of Science, Professor, 大学院・理学系研究科, 教授 (80192714)
川崎 清 独立行政法人水産総合研究センター, 中央水産研究所・海洋生産部, 室長(研究職)
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| Project Period (FY) |
2001 – 2003
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| Project Status |
Completed (Fiscal Year 2003)
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| Budget Amount *help |
¥13,500,000 (Direct Cost: ¥13,500,000)
Fiscal Year 2003: ¥3,800,000 (Direct Cost: ¥3,800,000)
Fiscal Year 2002: ¥4,200,000 (Direct Cost: ¥4,200,000)
Fiscal Year 2001: ¥5,500,000 (Direct Cost: ¥5,500,000)
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| Keywords | Kuroshio / Kuroshio Extension / Oyashio / ocean current / water mass / physical oceanography / oceanography / air-sea interaction |
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| Research Abstract |
We here hypothesize that variation of the cross-gyre transport from the subarctic to subtropical gyres producing NPIW induces long-term variations in the Kuroshio/Kuroshio Extension current system. In order to validate this hypothesis and detect the actually occurring formation processes of NPIW, we conducted data-analysis, numerical experiments and field observations; we successfully obtained extraordinary results. (1) Based on four surveys of water masses and ocean currents using CTD/LADCP observation, we revealed about 10Sv of cross-gyre Oyashio transport through the following two processes : direct cross-gyre transport along the western boundary and cross-subarctic front (SAF) process occurring along the offshore SAF due to isopycnal mixing. (2) The intrusion of western boundary currents across the wind-driven gyre boundary and related cross-gyre transport are realistically reproduced with a eddy-permitting three layer numerical models with realistic topography and annual mean wind
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stress, with special emphasis on the Oyashio southward intrusion and North Pacific intermediate Water (NPIW) formation. About 3Sv of the model diapycnal upwelling occurring due to strong tidal mixing along the Kurii islands induces a meridional-diapycnal overturning circulation. These results explain the observed features that about 4Sv of the cross-gyre Oyashio transport along the western boundary participate in the formation of NPIW. (3) High-resolution intensive observation using CTD/towed-CTD (MVP : Moving Vessel Profiler) and LADCP/ADCP were performed around the Kuroshio Extension. These observations revealed that intermediate-depth frontal waves with the wavelength of about 200km propagate in the downstream direction with the phase speed of 0.2m/s, amplifying the amplitude. The waves break down and mix the two water masses very efficiently in the downstream regions until 150E. A linear stability analysis reveals that the observed frontal waves are possibly the baroclinically unstable waves due to the coupling between the surface and intermediate-depth vorticity anomalies. The Oyashio water thus enhances intensive mixing and NPIW formation by entering into the Kuroshio Extension. Less
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