A numerical study of the wintertime circulation in the Bohai and Huanghai Seas

Le Kentang; Feng Ming; Wang Yue

doi:10.1007/BF02850822

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A numerical study of the wintertime circulation in the Bohai and Huanghai Seas

Updated：2023-05-16

- A numerical study of the wintertime circulation in the Bohai and Huanghai Seas
- Journal of Oceanology and Limnology Vol. 11, Issue 2, Pages: 149-160(1993)
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
- DOI：10.1007/BF02850822
  CLC：
- Published：1993
- Accepted：
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Kentang, L., Ming, F. & Yue, W. A numerical study of the wintertime circulation in the Bohai and Huanghai Seas., Chin. J. Ocean. Limnol. 11, 149–160 (1993). https://doi.org/10.1007/BF02850822
DOI：

Kentang, L., Ming, F. & Yue, W. A numerical study of the wintertime circulation in the Bohai and Huanghai Seas., Chin. J. Ocean. Limnol. 11, 149–160 (1993). https://doi.org/10.1007/BF02850822 DOI：

摘要

Abstract

The paper presents a numerical two-dimensional model (with a realistic sea basin and wind fields as exter nal forcing) to simulate the basic features of the wintertime circulation in the Bohai and Huanghai (Yellow) Seas (BHS) and to show how the circulation can be driven by wind. The main results can be summa rized as follows: (1) The basic features of the BHS wintertime circulation can be depicted by the wind-driven barotropic motion (2) The traditionally named Huanghai Sea Warm Current (HSWC) is actually generated by the north wind field

at least in winter. (3) The southward coastal current off the Korean west coast plays a more significant role in the southern Huanghai Sea wintertime circulation than traditionally believed. (4) Though the coastal landform and bottom topography play important roles in the wintertime BHS circulation pattern

the wind is a primary forcing.

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Keywords

references

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