| A NUMERICAL STUDY OF THE WINTERTIME CIRCULATION IN THE BOHAI AND HUANGHAI SEAS |
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| 引用本文： | 乐肯堂,冯明,王岳. A NUMERICAL STUDY OF THE WINTERTIME CIRCULATION IN THE BOHAI AND HUANGHAI SEAS[J]. 中国海洋湖沼学报, 1993, 11(2): 149-160. DOI: 10.1007/BF02850822 |
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| 作者姓名： | 乐肯堂 冯明 王岳 |
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| 作者单位： | Institute of Oceanology，Academia Snica，Qingdao 266071，Institute of Oceanology，Academia Snica，Qingdao 266071，Institute of Oceanology，Academia Snica，Qingdao 266071 |
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| 基金项目： | This work was supported by the National Natural Science Foundation of China ,4860242 |
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| 摘 要： | 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 summarized as follows (1) The basic features of the BHS wintertime circulation can be depicted by the wind-driven barotropi'c 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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| 收稿时间： | 1992-01-22 |
A numerical study of the wintertime circulation in the Bohai and Huanghai Seas |
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| Le Kentang,Feng Ming,Wang Yue. A numerical study of the wintertime circulation in the Bohai and Huanghai Seas[J]. Chinese Journal of Oceanology and Limnology, 1993, 11(2): 149-160. DOI: 10.1007/BF02850822 |
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| Authors: | Le Kentang Feng Ming Wang Yue |
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| Affiliation: | (1) Institute of Oceanology, Academia Sinica, 266071 Qingdao |
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| 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 summarized as follows (1) The basic features of the BHS wintertime circulation can be depicted by the wind-driven barotropi'c 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: | drculation Bohai and Huanghai Seas wintertime numerical study |
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