A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring

Zheng Yifang; Huang Weimin; Nakamura Yasuaki

doi:10.1007/BF02850861

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A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring

OriginalPaper | Updated：2023-05-16

- A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring
- A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring
- 海洋湖沼学报（英文） 1993年11卷第3期页码：276-284
- Affiliations：
  
  1. First Institute of Oceanography
  2. Seikai Fisheries Research
- Author bio：
- Funds：
- DOI：10.1007/BF02850861
  中图分类号：
- 纸质出版：1993
- Accepted：
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A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring[J]. 海洋湖沼学报（英文）, 1993,11(3):276-284.

Yifang, Z., Weimin, H. & Yasuaki, N. A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring., Chin. J. Ocean. Limnol. 11, 276–284 (1993). https://doi.org/10.1007/BF02850861
A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring[J]. 海洋湖沼学报（英文）, 1993,11(3):276-284. DOI： 10.1007/BF02850861.

Yifang, Z., Weimin, H. & Yasuaki, N. A preliminary analysis on the characteristics of the Kuroshio frontal eddy in the East China Sea in spring., Chin. J. Ocean. Limnol. 11, 276–284 (1993). https://doi.org/10.1007/BF02850861 DOI：

摘要

Abstract

The Kuroshio front eddy’s surface and sectional isothermal distribution characteristics were analyzed on the basis of observation data obtained in April 13–16 of 1989 in the East China Sea. It was found from the similarity between these isothermal distributions with those in January and beginning of June for the years 1986–1990 that the Kuroshio front eddy often occurred from March to the beginning of June. The Kuroshio front eddy movement in the East China Sea in spring was along two routes: the Okinawa Trough route

and the continental shelf slope route. The two moving routes both in the surface layer and in the section are described

their causes are discussed

and differences are compared.

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references

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