Simulation and analysis on seasonal variability of average salinity in the Yellow Sea

Ma Jian; Qiao Fangli

doi:10.1007/BF02842564

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Simulation and analysis on seasonal variability of average salinity in the Yellow Sea

OriginalPaper | Updated：2023-05-16

- Simulation and analysis on seasonal variability of average salinity in the Yellow Sea
- Simulation and analysis on seasonal variability of average salinity in the Yellow Sea
- 海洋湖沼学报（英文） 2004年22卷第3期页码：306-313
- Affiliations：
  
  1. The First Institute of Oceanography State Oceanic Administration SOA
  2. Key Laboratory of Marine Sciences and Numerical Modeling (MASNUM) SOA
- Author bio：
- Funds：
  
  Supported by the National Basic Research Program of China (No. G1999043809) and the National Science Foundation of China (No. 49736190).
- DOI：10.1007/BF02842564
  中图分类号：
- 纸质出版：2004
- Accepted：
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Simulation and analysis on seasonal variability of average salinity in the Yellow Sea[J]. 海洋湖沼学报（英文）, 2004,22(3):306-313.

Jian, M., Fangli, Q. Simulation and analysis on seasonal variability of average salinity in the Yellow Sea., Chin. J. Ocean. Limnol. 22, 306–313 (2004). https://doi.org/10.1007/BF02842564
Simulation and analysis on seasonal variability of average salinity in the Yellow Sea[J]. 海洋湖沼学报（英文）, 2004,22(3):306-313. DOI： 10.1007/BF02842564.

Jian, M., Fangli, Q. Simulation and analysis on seasonal variability of average salinity in the Yellow Sea., Chin. J. Ocean. Limnol. 22, 306–313 (2004). https://doi.org/10.1007/BF02842564 DOI：

摘要

Abstract

The CTD (conductivity

temperature and depth) data collected by six China-Korea joint cruises during 1996–1998 and the climatological data suggest that the seasonal variability of average salinity in the Yellow Sea (Sa) presents a general sinusoid pattern. To study the mechanism of the variability

annual cycles ofSa were simulated and a theoretical analysis based on the governing equations was reported. Three main factors are responsible for the variability: the Yellow Sea Warm Current (YSWC)

the Changjiang (Yangtze) River diluted water (YRDW) and the evaporation minus precipitation (E-P). From December to the next May

the variability ofSa is mainly controlled by the salt transportation of the YSWC. But in early July

the YSWC is overtaken and replaced by the YRDW which then becomes the most important controller in summer. From late September to November

the E-P gradually took the lead. The mass exchange north of the 37°N line is not significant.

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Keywords

references

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