A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation

Miao Jingbang; Liu Xingquan

doi:10.1007/BF02846499

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A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation

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- A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation
- A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation
- 海洋湖沼学报（英文） 1988年6卷第3期页码：216-226
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 1508 from the Institute of Oceanology, Academia Sinica
- DOI：10.1007/BF02846499
  中图分类号：
- 纸质出版：1988
- Accepted：
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A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation[J]. 海洋湖沼学报（英文）, 1988,6(3):216-226.

Jingbang, M., Xingquan, L. A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation., Chin. J. Ocean. Limnol. 6, 216–226 (1988). https://doi.org/10.1007/BF02846499
A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation[J]. 海洋湖沼学报（英文）, 1988,6(3):216-226. DOI： 10.1007/BF02846499.

Jingbang, M., Xingquan, L. A numerical study of the wintertime circulation in the Northern Huanghai Sea and the Bohai Sea part I: Basic characteristics of the circulation., Chin. J. Ocean. Limnol. 6, 216–226 (1988). https://doi.org/10.1007/BF02846499 DOI：

摘要

Abstract

A numerical model is developed to explain the response of the shelf sea to the abrupt imposition of a steady

secular mean windstream field and the basic characteristics of the wintertime circulation in the Northern Huanghai Sea (Yellow Sea) and the Bohai Sea by using equidistant

staggered grid points

an implicit finite difference scheme and our new “splitting computational method” of adjustment

development

and dissipation processes. So far as the major tendency of the circulation is concerned

the numerical result agrees with the observational data. The computational results show that the eastern anticyclonic and the western cyclonic circulations constitute the main body of the wintertime circulation in the Northern Huanghai Sea

and that the northern anticyclonic and the southern cyclonic circulations constitute the main body of the wintertime circulation in the Bohai Sea.

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Keywords

references

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