The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997

Luo Yi-yong; Bao Xian-wen; Wu De-xing

doi:10.1007/BF02844928

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The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997

OriginalPaper | Updated：2023-05-16

- The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997
- The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997
- 海洋湖沼学报（英文） 1998年16卷第4期页码：317-325
- Affiliations：
  
  Institute of Physical Oceanography
- Author bio：
- Funds：
  
  Project supported by the China-Japan Joint Investigation of Subtropical Circulations and Shandong Province's NSF (No. Q96E03138).
- DOI：10.1007/BF02844928
  中图分类号：
- 纸质出版：1998
- Accepted：
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The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997[J]. 海洋湖沼学报（英文）, 1998,16(4):317-325.

Yi-yong, L., Xian-wen, B. & De-xing, W. The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997., Chin. J. Ocean. Limnol. 16, 317–325 (1998). https://doi.org/10.1007/BF02844928
The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997[J]. 海洋湖沼学报（英文）, 1998,16(4):317-325. DOI： 10.1007/BF02844928.

Yi-yong, L., Xian-wen, B. & De-xing, W. The hydrographic features of the ocean region around the Ryukyu Islands during summer of 1997., Chin. J. Ocean. Limnol. 16, 317–325 (1998). https://doi.org/10.1007/BF02844928 DOI：

摘要

Abstract

Study of CTD data collected by theR/V DONG FANG HONG 2 in a 1997 summe cruise in the ocean region around the Ryukyu Islands showed: 1) the existence

in the upper layer

of a high salinity water (HSW) core at about 200 dbar

and a low salinity water (LSW) core

centered at about 700 dbar on the Pacific Ocean side of the Ryukyu Ridge

and located shallower on the East China Sea (ECS) side; 2) the existence

in the upper layer

of warm water regions (WWR) west of Amami Island and Ishigaki Island

and a cold water region (CWR) east of Okinawa Island; in the lower layer

of a CWR (WWR) southwest (southeast) of Okinawa Island; 3) the intrusion of North Pacific Intermediate Water into the ECS through the Kerama Trench located south of Okinawa Island and the strait east of Taiwan Island.

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references

Nitani, H., 1972. Beginning of the Kuroshio.In: Kuroshio, edited by H. Stommel and K. Yoshido, University of Tokyo Press, p. 129–163.

Pu Yongxiu, Su Yufen, 1990. The hydrographic features of the area around the island chain from Miyaka-Jima Island to Yakushima Island during May–June of 1986. Proceedings of Investigation of Kuroshio (I). China Ocean Press, Beijing, p. 137–148.

Su Jilan, Guan Bingxian, Jing Jingzhong, 1990. The Kuroshio. Part I: Physical Features,Oceanogr. Wlar. Biol. Annu. Rev.,28: 11–71.

Sun Xiangping, 1987. Analysis of the surface path of the Kuroshio in the East China Sea. Essays on the Investigation of Kuroshio. China Ocean Press, Beijing, p. 1–14.

Wang Yuanpei, Sun Xiangping, 1990. A study on the features of the Ryukyu current. Proceedings of Investigation of Kuroshio (II). China Ocean Press, Beijing, p. 237–245.

Yuan Yaochu, Pan Ziqin, 1994. Variability of the Kuroshio in the East China Sea and the currents east of the Ryukyu Islands. Proceedings of China-Japan Joint Symposium of the Cooperative Research on the Kuroshio. China Ocean Press, Beijing, p. 121–144.

Yu Honghua, Su Jilan, Miao Yutian et al., 1994. Low salinity water core of Kuroshio in the East China Sea and intrusion of western boundary current east of the Ryukyu Islands. Proceedings of China-Japan Joint Symposium of the Cooperative Research on the Kuroshio. China Ocean Press, Beijing, p. 145–163.

Yu Honghua, Su Jilan, 1992. Characteristic Analysis of the Anticyclonic Gyres in the Area of the Kunoshio South of the East China Sea. Proceedings of Investigation of Kuroshio (IV). China Ocean Press, Beijing, p. 228–238.

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