Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982

Zhu Jianrong; Qi Dingman; Xiao Chengyou

doi:10.1007/BF02842556

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Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982

OriginalPaper | Updated：2023-05-16

- Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982
- Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982
- 海洋湖沼学报（英文） 2004年22卷第3期页码：250-255
- Affiliations：
  
  1. State Key Laboratory of Estuarine and Coastal Research East China Normal University
  2. Center of Estuarine and Coastal Science Research Science Research College of Transport Bureau
- Author bio：
- Funds：
  
  Supported by the Major State Research Program of China (No. G1999043803), the Teaching and Research Award Fund for outstanding Young Teachers in Higher Education. Institutions of MOD, P. R. China, and the National Science Foundation of China (No. 49876002).
- DOI：10.1007/BF02842556
  中图分类号：
- 纸质出版：2004
- Accepted：
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Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982[J]. 海洋湖沼学报（英文）, 2004,22(3):250-255.

Jianrong, Z., Dingman, Q. & Chengyou, X. Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982., Chin. J. Ocean. Limnol. 22, 250–255 (2004). https://doi.org/10.1007/BF02842556
Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982[J]. 海洋湖沼学报（英文）, 2004,22(3):250-255. DOI： 10.1007/BF02842556.

Jianrong, Z., Dingman, Q. & Chengyou, X. Observed residual currents off the Changjiang (Yangtze) River mouth in summertime of 1959 and 1982., Chin. J. Ocean. Limnol. 22, 250–255 (2004). https://doi.org/10.1007/BF02842556 DOI：

摘要

Abstract

Data taken in two large scale ocean observations in China in summer 1959 and 1982 were used to analyze the residual current off the Changjiang (Yangtze) River mouth. The currents at surface off the mouth in July 1959 and 1982 flow northeastward and eastward due to the river discharge

the current speed was larger in 1982 than in 1959. All the bottom currents flow landward due to baroclinic effect. The surface current was controlled by the river runoff and the Taiwan Warm Current (TWC). A return current at surface off the mouth was observed in September 1959. In general

the bottom currents were controlled by the TWC in most study area in addition to the runoff near the mouth. Although driven by 3-D model with the monthly averaged forces (river discharge

wind stress

baroclinic effect

open boundary water volume flux and tidal mixing) in August

the simulated circulations were basically consistent with the observed ones with episodic time manner.

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references

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