Vertical structure and seasonal variation of tidal and residual currents in the northern Huanghai Sea

SONG Jun GUO Junru QIAO Lulu MU Lin YAO Zhigang LIU Yang LI Huan BAO Xianwen SUN Xiaoyan GAO Jia

SONGJun, GUOJunru, QIAOLulu, MULin, YAOZhigang, LIUYang, LIHuan, BAOXianwen, SUNXiaoyan, GAOJia. Vertical structure and seasonal variation of tidal and residual currents in the northern Huanghai Sea[J]. 海洋学报英文版, 2011, (5): 14-22. doi: 10.1007/s13131-011-0143-2
引用本文: SONGJun, GUOJunru, QIAOLulu, MULin, YAOZhigang, LIUYang, LIHuan, BAOXianwen, SUNXiaoyan, GAOJia. Vertical structure and seasonal variation of tidal and residual currents in the northern Huanghai Sea[J]. 海洋学报英文版, 2011, (5): 14-22. doi: 10.1007/s13131-011-0143-2
SONG Jun, GUO Junru, QIAO Lulu, MU Lin, YAO Zhigang, LIU Yang, LI Huan, BAO Xianwen, SUN Xiaoyan, GAO Jia. Vertical structure and seasonal variation of tidal and residual currents in the northern Huanghai Sea[J]. Acta Oceanologica Sinica, 2011, (5): 14-22. doi: 10.1007/s13131-011-0143-2
Citation: SONG Jun, GUO Junru, QIAO Lulu, MU Lin, YAO Zhigang, LIU Yang, LI Huan, BAO Xianwen, SUN Xiaoyan, GAO Jia. Vertical structure and seasonal variation of tidal and residual currents in the northern Huanghai Sea[J]. Acta Oceanologica Sinica, 2011, (5): 14-22. doi: 10.1007/s13131-011-0143-2

Vertical structure and seasonal variation of tidal and residual currents in the northern Huanghai Sea

doi: 10.1007/s13131-011-0143-2
基金项目: The Public Science and Technology Research Funds Projects of Ocean under contract Nos 200905001 and 201005019; the State Basic Research Program of China under contract No. 2005CB422303; the National Natural Science Foundation of China under contract No. 41006002.

Vertical structure and seasonal variation of tidal and residual currents in the northern Huanghai Sea

  • 摘要: Analysis of tidal current and sea level has been made based on the observations from the summer of 2006 to the winter of 2007, respectively. The result indicates that a two-layer structure of residual current exists in summer, with its upper layer going northwestward and the lower layer southeastward. In addition, some strong residuals exist in the neighboring depth of the pycnocline during the current period of astronomical tide. In winter, except some individual layersthe residual currents mostly direct to the northwest, from which we can see the fluctuation of abnormal sea-level and the appearance of associated current because of the changes of the wind field. The analysis of tidal ellipse indicates that the direction of the maximum semidiurnal component is clockwise from summer to winter, with an angle of 16°-18°. Moreover, in summer the semidiurnal component rotates with depth clockwise while the diurnal component counterclockwise. However, the vertical structure is almost homogeneous in winter.
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  • 收稿日期:  2011-01-24
  • 修回日期:  2011-06-14

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