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Autumn intensification of the Ryukyu Current during 2003-2007 被引量:4

Autumn intensification of the Ryukyu Current during 2003-2007
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摘要 Inverse calculations using data from 16 repeat hydrographic transects collected from April 2003 to June 2007 have yielded velocity structures and volume transports(VTs) of the Ryukyu Current in the region east of the northern Ryukyu Islands.The inverse calculation results show that the Ryukyu Current is dominated by a subsurface velocity core with maximum velocities from 15.1 to 80.0 cm/s,whose positions vary between 110 and 600 dbar and 27.2°-28.2°N along the transect.The mean velocity exhibits a subsurface velocity core with a maximum value of 24.6 cm/s at 326 dbar depth,a VT of 14.0 Sv(1 Sv≡106 m3/s),a vertical dimension of 800 m,and a horizontal dimension of 60 km.The seasonal mean velocities show that the Ryukyu Current is stronger in autumn than in other seasons.It is suggested that this seasonal variation is coincident with the intensification of the anticyclonic eddy south of Shikoku,Japan. Inverse calculations using data from 16 repeat hydrographic transects collected from April 2003 to June 2007 have yielded velocity structures and volume transports(VTs) of the Ryukyu Current in the region east of the northern Ryukyu Islands.The inverse calculation results show that the Ryukyu Current is dominated by a subsurface velocity core with maximum velocities from 15.1 to 80.0 cm/s,whose positions vary between 110 and 600 dbar and 27.2°-28.2°N along the transect.The mean velocity exhibits a subsurface velocity core with a maximum value of 24.6 cm/s at 326 dbar depth,a VT of 14.0 Sv(1 Sv≡106 m3/s),a vertical dimension of 800 m,and a horizontal dimension of 60 km.The seasonal mean velocities show that the Ryukyu Current is stronger in autumn than in other seasons.It is suggested that this seasonal variation is coincident with the intensification of the anticyclonic eddy south of Shikoku,Japan.
出处 《Science China Earth Sciences》 SCIE EI CAS 2010年第4期603-609,共7页 中国科学(地球科学英文版)
基金 supported by National Natural Science Foundation of China (Grant Nos.40776021,40706018) National Basic Research Program of China (Grant No.2006CB400603) National High Technology Research and Development Program of China (Grant No.2006AA09Z102) JSPS KAKENHI (Grant No.21310012)
关键词 Ryukyu CURRENT inverse technique SUBSURFACE maximum velocity core volume TRANSPORTS SEASONAL variation Ryukyu Current inverse technique subsurface maximum velocity core volume transports seasonal variation
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参考文献21

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