A homogeneous model of upper layer circulation in Indo-Pacific region

Wang Fan; Hu Dun-xin

doi:10.1007/BF02850680

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A homogeneous model of upper layer circulation in Indo-Pacific region

OriginalPaper | Updated：2023-05-16

- A homogeneous model of upper layer circulation in Indo-Pacific region
- A homogeneous model of upper layer circulation in Indo-Pacific region
- 海洋湖沼学报（英文） 1997年15卷第2期页码：118-124
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 2957 from the Institute of Oceanology, Chinese Academy of Sciences.;Project 49176255 supported by NSFC.
- DOI：10.1007/BF02850680
  中图分类号：
- 网络首发：2013-01-31，
  
  纸质出版：1997
- Accepted：
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A homogeneous model of upper layer circulation in Indo-Pacific region[J]. 海洋湖沼学报（英文）, 1997,15(2):118-124.

Fan, W., Dun-xin, H. A homogeneous model of upper layer circulation in Indo-Pacific region., Chin. J. Ocean. Limnol. 15, 118–124 (1997). https://doi.org/10.1007/BF02850680
A homogeneous model of upper layer circulation in Indo-Pacific region[J]. 海洋湖沼学报（英文）, 1997,15(2):118-124. DOI： 10.1007/BF02850680.

Fan, W., Dun-xin, H. A homogeneous model of upper layer circulation in Indo-Pacific region., Chin. J. Ocean. Limnol. 15, 118–124 (1997). https://doi.org/10.1007/BF02850680 DOI：

摘要

Abstract

A homogeneous model is proposed to study the upper layer circulation in the Indo-Pacific region

the sources of the Indonesian throughflow (TF) and the North Equatorial Countercurrent (NECC)

and the relations of the two with the North Equatorial Current (NEC) and the South Equatorial Current (SEC). The results revealed that the upper layer circulaton

as part of the Pacific Ocean general circulation

is mainly controlled by geostrophic balance; that the NECC's volume transport is mainly supplied by the NEC

and its variation has closer relation to the NEC than the SEC; that the TF

whose volume transport is jointly supplied by the NEC through the Mindanao Current (MC) and the SEC

with the NEC being the first source

has significant influence on the circulation structure; and that a large Celebes Sea cyclonic circulation not mentioned elsewhere so far

exists in the calculated results.

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Keywords

references

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