HYDRODYNAMIC RESPONSE OF CHENIER COAST TO STORM SURGES ON THE ABANDONED YELLOW RIVER DELTA PLAIN
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摘要: 渤海湾西南岸大口河口至马颊河口一线分布着大口河岛、高坨子、棘家堡子和汪子岛等贝壳堤(岛)。以2003年10月10-12日发生的50年一遇的温带风暴潮为动力条件,结合对历史文献、海图、卫星影像等资料的分析,利用FVCOM和SWAN数值模式,耦合模拟了黄河废弃三角洲不同时期代表性岸线形态约束下贝壳堤近岸的波浪、潮流等动力响应特征。贝壳堤的规模、形态、分布等受特殊的岸线形态、海滩物质组成以及由ENE、NE强风驱动的风暴潮动力场等所控制。由于黄骅港和滨州港超长防波堤的掩护作用,在同等风暴潮强度下,贝壳堤近岸的潮位、流速和波高均有所减小,有利于贝壳堤的加积和稳定性。Abstract: Along the coastline from the Dakou river mouth to Taoer river mouth in SW Bohai Bay,chenier ridges have been found at the places of Dakouhedao,Gaotuozi,Jijiapuzi and Wangzidaos.Historical documents, sea charts and satellite images show that the characteristics of the coastline were formed by the shifting of the Yellow River mouth and the consequent evolution of the delta plain.A storm surge,which came once every 50 years,happened on October 10-12,2003.The numerical model of FVCOM +SWAN is adopted in this paper to simulate and investigate the nearshore wind-driven wave,and flow fields for different coastline configurations.The results demonstrate that the dimensions,shapes and distributions of chenier ridges are controlled and reworked by coastline configurations,material sources and ENE,NE winddriven hydrodynamics.The intensity of the storm surge,flow power and wave height will be reduced moderately by the chenier ridges due to the sheltering effect of the long breakwaters of the Huanghua Port and the Binzhou Port.This study will help preserve the existing chenier system and favor the formation of new chenier ridge.
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Key words:
- chenier ridge /
- abandoned delta coast /
- storm surge /
- FVCOM /
- SWAN
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[1] 黄世光.套尔河湾海域泥沙冲淤特征——兼论黄河改道后三角洲的冲淤演化[J].海洋与湖沼,1993,24(2):197-204.
[HUANG Shiguang.Erosion and accumulation in the adjacent area of the Taoerhe Bay-with emphasis on the erosion and accumulation of the Huanghe River delta after its shifted course[J].Oceanologia et Limnologia Sinica,1993,24(2):197-204.]
[2] 岳军,Dong Yue,张宝华,等.渤海湾西岸的几道贝壳堤[J].地质学报,2012,86(3):522-534.
[YUE Jun,DONG Yue, ZHANG Baohua et al.A few of barrier sand bars on the west coast of Bohai Bay[J].Acta Geologica Sinica,2012,86(3):522-534.]
[3] 杜廷芹,黄海军,王珍岩,等.黄河三角洲北部贝壳堤岛的近期演变[J].海洋地质与第四纪地质,2009,29(3):23-29.
[DU Yanqin,HUANG Haijun,WANG Zhenyan,et al.Evolution of the shell ridge islands on the northern Yellow River Delta[J].Marine Geology and Quaternary Geology,2009,29(3):23-29.]
[4] 刘志杰.鲁北贝壳滩脊沉积及发育演化研究[D].青岛:中国海洋大学,2004.[LIU Zhijie.The sedimentary characteristics and evolution of shell ridge,north coast of Shandong Province[D].Qingdao:Ocean University of China,2004.]
[5] 罗刚,杨希宏.黄骅港一期工程总平面布置格局的论证[J].中国港湾建设,2003,122(1):5-8.
[LUO Gang,YANG Xihong. Verification of general plan layout for phase I works at Port Huanghua[J].China Harbor Engineering,2003,122(1):5-8.]
[6] [7] 冯海防.黄骅港潮流、泥沙数值模拟及工程影响分析[D].上海:同济大学,2009.[FENG Haifang.Numerical modeling tidal and sediment transport and analysis of engineering influences[D].Shanghai:Tongji University,2009.]
[8] 薛春汀.渤海西岸漳卫新河口至徒骇河口海岸地貌成因[J]. 海洋科学进展,2011,29(3):330-338.
[XUE Chunting.Origin of coastal landforms from the Zhangweixin river mouth to theTuhairiver mouth along the west Coast of the Bohai Sea[J].Advances in Marine Sciences,2011,29(3):330-338.]
[9] 庄振业,许卫东,李学伦.渤海南岸6000年来的岸线演变[J]. 青岛海洋大学学报,1991,21(2):99-110.
[ZHUANG Zhenye, XU Weidong,LI Xuelun.The coastline evolution of the south coast of the Bohai Sea since 6kaBP[J].Journal of Qingdao Ocean University,1991,21(2):99-110.]
[10] 王宗涛,冯怀珍,邱建立.关于套尔河成因以及滨州港建设的几个问题[J].海洋通报,1995,14(3):81-85.
[WANG Zongtao, FENG Huaizhen,QIU Jianli.Cause of formation of Taoer river and some problems in construction of Binzhou Port[J].Marine Science Bulletin,1995,14(3):81-85.]
[11] 崔承琦,施建堂,张庆德.古代黄河三角洲海岸的现代特征-黄河三角洲潮滩时空谱系研究I[J].海洋通报,2001,20(1):46-52.
[CUI Chengqi,SHI Jiantang,ZHANG Qingde.Modern characteristics of the ancient Yellow River delta coast-Research on the space-time lineage of the Yellow River deltaflat coast I[J].Marine Science Bulletin,2001,20(1):46-52.]
[12] 曾宜.黄骅港外航道整治工程及航道骤淤防治技术[J].神华科技,2009,27(1):64-67.
[ZENG Yi.The Harnessing of Outer Channel of Huanghua Port and Sediment Control Techniques[J].Shenhua Science and Technology,2009,27(1):64-67.]
[13] Chen C S,Liu H D,and Beardsley R C.An unstructuredgrid, finite-volume,three-dimensional, primitiveequation ocean model:application to coastal ocean and estuaries[J].Journal of Atmospheric and Oceanic Technology,2003, 20:159-186.
[14] Warner J C,Sherwood C R,Signell R P,et al.Development of a three-dimensional,regional,coupled wave,current,and sediment-transportmodel[J].Computers and Geosciences, 2008,34:1284-1306.
[15] The SWAN team.User Manual.SWAN Cycle Ⅲ version 41.01,2014.
[16] 聂庆林,武俊岭,玉洪超,等.鲁北地区"2003.10"特大暴雨分析[J].水文,2006,26(5):93-94.
[NIE Qinglin,WU Junling, YU Hongchao,et al.Analysis of "2003.10" severe rainstorm in northern Shandong Province[J].Journal of China Hydrology,2006,26(5):93-94.]
[17] 于亮.考虑波流耦合作用的渤海湾风暴潮三维数值模拟[D]. 天津:天津大学,2010.[YU Liang.The 3D numerical model of storm surge of Bohai Bay incorporating wave-curremtcoupling[D].Tianjin:Tianjin University,2010.]
[18] 夏东兴,王德邻,吴桑云,等.鲁北沿岸贝壳堤的地质学意义[J].黄渤海海洋,1991,9(3):19-24.
[XIA Dongxing, WANG Deling,WU Sangyun.The geological significance of the cheniers along the coast of northern Shandong Province[J].Journal of Oceanography of Huanghai & Bohai Sea, 1991,9(3):19-24.]
[19] 王强,袁桂邦,张熟,等.渤海湾西岸贝壳堤堆积与海陆相互作用[J].第四纪研究,2007,27(5):775-786.
[WANG Qiang,YUAN Guibang,ZHANG,Shu,et al.Shelly ridge accumulation and sea-land interaction on the west coast of the Bohai Bay[J].Quaternary Sciences,2007,27(5):775-786.]
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