Some features of circulation in the southern Huanghai Sea

Tang Yuxiang; Zou Emei; Lie Heung-Jae; Lie Jae-Hank

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Tang Yuxiang, Zou Emei, Lie Heung-Jae, Lie Jae-Hank. Some features of circulation in the southern Huanghai Sea[J]. Haiyang Xuebao, 2000, 22(1): 1-16.

Citation:

Tang Yuxiang, Zou Emei, Lie Heung-Jae, Lie Jae-Hank. Some features of circulation in the southern Huanghai Sea[J]. Haiyang Xuebao, 2000, 22(1): 1-16.

Tang Yuxiang, Zou Emei, Lie Heung-Jae, Lie Jae-Hank. Some features of circulation in the southern Huanghai Sea[J]. Haiyang Xuebao, 2000, 22(1): 1-16.

Citation:

Tang Yuxiang, Zou Emei, Lie Heung-Jae, Lie Jae-Hank. Some features of circulation in the southern Huanghai Sea[J]. Haiyang Xuebao, 2000, 22(1): 1-16.

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Some features of circulation in the southern Huanghai Sea

1.
Key Laboraeq of Marine Science and Numerical Modeling, State Oceanic Administraction; First Institute of Oceanography, State Oceanic Administration, Qingdao 266003
2.
Korea Ocean Reunrch & Development Institute, Ausan, Korea

Received Date: 1998-12-30
Rev Recd Date: 1999-03-21

Abstract

Abstract

Some features of circulation in the southern Huanghai Sea (SHS) are analyzed on the basis of the observations of the China-Korea Joint Investigation of Ocean Circulation Dynamics in the SHS in the recent years and historical data.The main results are as follows:(1) The circulation in the SHS shows obvious seasonal variation.The basic patterns of the circulation are quite different in winter and summer.(2) The path and the strength of the Huanghai Warm Current (HWC) has certain interannual variations.Analyses indicate that the path of the HWC was obviously to the west of the trough in the winter of 1997,but went toward the north along the trough in the winter cd 1986.(3) The HWC is not a direct branch of the Tsushima Warm Current.The HWC water is a mixture of the Tsushima Warm Current water and the continental shelf water,but originates mainly from the frontal area west of Cheju-do.(4) The summertime circulations are basically composed of a hasinscale counterclockwise flow in both surface and bottom layers.However,several smaller cyclonic and anticyclonic systems appear in the larger couunterclockwise circulation.There is no obvious indications that the high temperature-salinity water enters into the eastern Huanghei Sea from the sea area adjacent to Cheju-do in the surface and bottom layer.
- Southern Huanghai Sea,
- circulation,
- features

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References(23)

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