The surface path of the Kuroshio Extension’s western sector and the eddies on both sides

Sun Xiangping; Wang Yuanpei; Yuan Qike

doi:10.1007/BF02846261

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The surface path of the Kuroshio Extension’s western sector and the eddies on both sides

OriginalPaper | Updated：2023-05-16

- The surface path of the Kuroshio Extension’s western sector and the eddies on both sides
- The surface path of the Kuroshio Extension’s western sector and the eddies on both sides
- 海洋湖沼学报（英文） 1989年7卷第4期页码：300-311
- Affiliations：
  
  First Institute of Oceanography
- Author bio：
- Funds：
- DOI：10.1007/BF02846261
  中图分类号：
- 纸质出版：1989
- Accepted：
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The surface path of the Kuroshio Extension’s western sector and the eddies on both sides[J]. 海洋湖沼学报（英文）, 1989,7(4):300-311.

Xiangping, S., Yuanpei, W. & Qike, Y. The surface path of the Kuroshio Extension’s western sector and the eddies on both sides., Chin. J. Ocean. Limnol. 7, 300–311 (1989). https://doi.org/10.1007/BF02846261
The surface path of the Kuroshio Extension’s western sector and the eddies on both sides[J]. 海洋湖沼学报（英文）, 1989,7(4):300-311. DOI： 10.1007/BF02846261.

Xiangping, S., Yuanpei, W. & Qike, Y. The surface path of the Kuroshio Extension’s western sector and the eddies on both sides., Chin. J. Ocean. Limnol. 7, 300–311 (1989). https://doi.org/10.1007/BF02846261 DOI：

摘要

Abstract

The surface path of the Kuroshio Extension’s western sector and the eddies on both sides are systematically analysed based on the GEK-measured surface current and temperature-salinity data from 1955–1985. The main results are shown as follows:1) According to the position and the features of distribution pattern

the surface path of the Kuroshio Extension’s western sector is classified into two kinds (straight and meander) and seven types (f. ne

Ui or Vi

Vdi or Udi

f+v). The straight kind accounts for 1/3 and the meander kind accounts for 2/3. 2) The warm eddies on the northern side originate mostly from the area off Sanriku and Joban of Japan. Their moving paths lie in two patterns: Pattern I

eddy moves northeastward or northward; Pattern II

eddy rotates about the original area. The cold eddies on the southern side originate mainly from the area off Boso Peninsula. Their moving paths also lie in two patterns: Pattern III. eddy moves from west to east; Pattern IV

eddy moves from north to south.

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references

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