| Project/Area Number |
07454112
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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 | Kyushu University |
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Principal Investigator |
IMAWAKI Shiro Kyushu University, Res.Inst.for Appl.Mech., Professor, 応用力学研究所, 教授 (40025474)
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| Co-Investigator(Kenkyū-buntansha) |
KANEKO Arata Hiroshima University, Faculty of Engineering, Professor, 工学部, 教授 (10038101)
UMATANI Shin-ichiro Kyushu University, Res.Inst.for Appl.Mech., Research Associate, 応用力学研究所, 助手 (30112353)
OSTROVSKII Alexander Kyushu University, Res.Inst.for Appl.Mech., Associate Professor, 応用力学研究所, 助教授 (70243962)
TAKEMATSU Masaki Kyushu University, Res.Inst.for Appl.Mech., Professor, 応用力学研究所, 教授 (50038535)
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| Project Period (FY) |
1995 – 1996
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| Project Status |
Completed (Fiscal Year 1996)
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| Budget Amount *help |
¥6,400,000 (Direct Cost: ¥6,400,000)
Fiscal Year 1996: ¥2,000,000 (Direct Cost: ¥2,000,000)
Fiscal Year 1995: ¥4,400,000 (Direct Cost: ¥4,400,000)
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| Keywords | Kuroshio / transport / ADCP |
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| Research Abstract |
Intensive surveys of the Kuroshio off Shikoku were carried out during 1993-1995 along a subsatellite track of the altimeter satallite TOPEX/POSEIDON.Hydrographic surveys and towed-ADCP (acoustic Doppler current profiler) surveys were carried out repeatedly along the line. Data from those observations as well as moored current measurements were analyzed synthetically. The following results were obtained ;
(1) Two modes of the surface Kuroshio were detected by the repeated towed-ADCP surveys : one is the Kuroshio flowing very close to the coast and the other is that flowing far offshore.
(2) Very strong flows (up to 100 cm/sec) and very strong vertical shears (stronger than 0.01 sec^<-1>) were observed around 300m depth by a moored-ADCP.
(3) Generally, geostrophic shears estimated from the repeated hydrographic survey data compare well with vertical shears obtained from the direct current measurement data, but the abovementioned strong shears were not able to be estimated from the present hydrographic data.
(4) Tide gauge data at a coastal station were compared with satellite altimetry data successfully and found to represent well the sea level fluctuations on the coastal side of the Kuroshio.
(5) On the basis of combination of those in situ oceanographic data and satellite altimetry data, a three-year long time series of the Kuroshio transport was obtained with ten-day resolution. The results show that there are not apparent seasonal signals in the estimated fluctuations, which fact gives us a very important and interesting task in the future.
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