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PU YONGXIU,XU XlAOYUN. 1987. THE KUROSHIO (ON THE PN SECTION) IN THE EAST CHINA SEA DURING 1972-1983. Acta Oceanologica Sinica, (1):37－45
THE KUROSHIO (ON THE PN SECTION) IN THE EAST CHINA SEA DURING 1972-1983
THE KUROSHIO (ON THE PN SECTION) IN THE EAST CHINA SEA DURING 1972-1983
Received:April 06, 1985  Revised:October 04, 1985
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Author NameAffiliation
PU YONGXIU The Second Institute of Oceanography, State Oceanic Adiministration Hangzhou 
XU XlAOYUN The Second Institute of Oceanography, State Oceanic Adiministration Hangzhou 
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Abstract:
      The current elements of the Kuroshio in the East China Sea are analysed and discussed using the temperature-salinity and GEK data of the PN section obtained during 1972-1983.The calculations have proved (ⅰ) that the 12-year's mean volume transport of the Kuroshio at PN in the 0-800 m layer is about 20×106m3/s; (ⅱ) that the mean volume transport has seasonal variations, i.e.slightly stronger in spring and summer than in the other seasons; and (ⅲ) that the period of high-volume transport thereof corresponds to the appearance of a meander of the Kuroshio south of Japan.It is also discovered that this Kuroshio meander usually appears after a sharp increase in such volume transport.Finally, the differences of the Kuroshio volume transport between the PN, E and Suao-Yonakuni-jima sections are discussed.
中文摘要:
      The current elements of the Kuroshio in the East China Sea are analysed and discussed using the temperature-salinity and GEK data of the PN section obtained during 1972-1983.The calculations have proved (ⅰ) that the 12-year's mean volume transport of the Kuroshio at PN in the 0-800 m layer is about 20×106m3/s; (ⅱ) that the mean volume transport has seasonal variations, i.e.slightly stronger in spring and summer than in the other seasons; and (ⅲ) that the period of high-volume transport thereof corresponds to the appearance of a meander of the Kuroshio south of Japan.It is also discovered that this Kuroshio meander usually appears after a sharp increase in such volume transport.Finally, the differences of the Kuroshio volume transport between the PN, E and Suao-Yonakuni-jima sections are discussed.
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