Analysis of largest tidal range in radial sand ridges southern Yellow Sea

Ding Xianrong; Kang Yanyan; Mao Zhibing; Sun Yulong; Li Sen; Gao Xuan; Zhao Xiaoxu

doi:10.3969/j.issn.0253-4193.2014.11.002

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Ding Xianrong, Kang Yanyan, Mao Zhibing, Sun Yulong, Li Sen, Gao Xuan, Zhao Xiaoxu. Analysis of largest tidal range in radial sand ridges southern Yellow Sea[J]. Haiyang Xuebao, 2014, 36(11): 12-20. doi: 10.3969/j.issn.0253-4193.2014.11.002

Citation:

Ding Xianrong, Kang Yanyan, Mao Zhibing, Sun Yulong, Li Sen, Gao Xuan, Zhao Xiaoxu. Analysis of largest tidal range in radial sand ridges southern Yellow Sea[J]. Haiyang Xuebao, 2014, 36(11): 12-20. doi: 10.3969/j.issn.0253-4193.2014.11.002

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Analysis of largest tidal range in radial sand ridges southern Yellow Sea

doi: 10.3969/j.issn.0253-4193.2014.11.002

1.
College of Hydrology and Water Resources, Hohai University, Nanjng 210098, China
2.
College of Harbor, Coastal and Offshore Engineering, Hohai University, Nanjng 210098, China
3.
School of Earth Sciences and Engineering, Hohai University, Nanjng 210098, China

Received Date: 2013-04-17

Abstract

Abstract

The largest tidal range 9.39 m was observed on October 17, 2012 at Xintiaoyugang station which is one of 4 tide-gauge stations along coast of the radial sand ridges, southern Yellow Sea. It confirms that the historical tidal range 9.28 m in Xiaoyangkou in 1980's is reliable and the largest tidal range record in this sea area is renewed. Reasons of the largest tidal range are expressed from two aspects. One is "movable standing tidal wave" that is the hydrodynamic cause by hydrodynamic simulation modeling. The other is "the water diversion"(Erfenshui) that is the dynamic geomorphic reason by remote sensing interpretation. As the results, "Jump Rope" effect of the synchronous water level along Tiaozini tidal flat and the largest tidal range of 9.39 m is reasonable and effective. Even more, the maximum tidal range in this area could be 9.62 m if statistical method can be changed. The largest tidal range of radial sand ridges in this paper has reference value and innovation of the tidal characteristics in the whole coast of China.
- radial sand ridges,
- the largest tidal range,
- movable standing tidal wave,
- Tiaozini

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References

刘爱菊,尹逊福,卢铭. 黄海潮汐特征Ⅰ [J]. 黄渤海海洋,1983,1(2): 1-7.

沈育疆. 东中国海潮汐数值计算[J]. 山东海洋学院学报,1980,10(3): 26-35.

任美锷. 江苏省海岸带和海涂资源综合调查报告[M]. 北京: 海洋出版社,1986: 25.

王颖,朱大奎. 海岸地貌学[M]. 北京: 高等教育出版社,1994: 27-28.

王颖. 黄海陆架辐射沙脊群[M]. 北京: 中国环境科学出版社,2002: 31.

张长宽. 江苏省近海海洋环境资源基本现状[M]. 北京: 海洋出版社,2013: 91-93.

张东生,张君伦. 黄海海底辐射沙洲区的M₂潮波[J]. 河海大学学报,1996,24(5): 35-40.

陶建峰,张东生,龚政. 江苏近海潮汐潮流的数值模拟[C]//第十四届中国海洋(岸)工程学术讨论会论文集. 2009: 559-562.

Yan Y X,Zhu Y L,Xue H C. Hydromechanics for the formation and development of radial sandbanks (Ⅰ)--Plane characteristics of tidal flow[J]. Science in China (Series D),1999,42(1): 13-21.

Yan Y X,Song Z Y,Xue H C,et al. Hydromechanics for the formation and development of radial sandbanks (Ⅱ)--Vertical characteristics of tidal flow[J]. Science in China (Series D),1999,42(1): 22-29.

Zhang C K,Zhang D S,Zhang J L,et al. Tidal current-induced formation-storm-induced change-tidal current-induced recovery--Interpretation of depositional dynamics of formation and evolution of radial sand ridges on the Yellow Sea seafloor[J]. Science in China (Series D),1999,42(1): 1-12.

吴德安,严以新,马林艺,等. 江苏辐射沙洲海域最大可能潮差的计算与分析[J]. 大连海事大学学报,2008,34(4): 75-78.

陈红霞,华锋,袁业立. 中国近海及临近海域海浪的季节特征及其时间变化[J]. 海洋科学进展,2006,24(4): 407-415.

中华人民共和国交通运输部搜救中心. 海洋气象·近海海区天气预报(12年10月17日14时)[EB/OL].(2012-10-17)[2013-12-05]. http://www.moc.gov.cn/zizhan/siju/soujiuzhongxin/haiyangqixiang/201210/t20121017_1313146.html.

Warren I R,Bach H K. MIKE 21: a modelling system for estuaries,coastal waters and seas [J]. Environmental Software,1992,7(4): 229-240.

Smagorinsk Y J. General circulation experiments with the primitive equations Ⅰ: the basic experiment[J]. Monthly Weather Review,1963,91(3): 99-164.

陶建峰,张长宽. 黄海辐射沙脊群海域水环境数值模拟研究[J]. 河海大学学报: 自然科学版,2005,33(4): 472-475.

丁贤荣,康彦彦,葛小平,等. 辐射沙脊群条子泥动力地貌演变遥感分析[J]. 河海大学学报:自然科学版,2011,39(2): 231-236.

孟德润,田光耀,刘雁春. 海洋潮汐学[M]. 北京: 海潮出版社,1993.

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