A numerical study on the circulation and tide in a zigzag bay

YU Huaming WANG Zhaohua KUANG Liang WANG Lu BAO Xianwen WU He WANG Xin DENG Xiaodong

YUHuaming, WANGZhaohua, KUANGLiang, WANGLu, BAOXianwen, WUHe, WANGXin, DENGXiaodong. 曲折海湾中潮汐和环流的数值研究[J]. 海洋学报英文版, 2015, 34(1): 119-128. doi: 10.1007/s13131-015-0604-0
引用本文: YUHuaming, WANGZhaohua, KUANGLiang, WANGLu, BAOXianwen, WUHe, WANGXin, DENGXiaodong. 曲折海湾中潮汐和环流的数值研究[J]. 海洋学报英文版, 2015, 34(1): 119-128. doi: 10.1007/s13131-015-0604-0
YU Huaming, WANG Zhaohua, KUANG Liang, WANG Lu, BAO Xianwen, WU He, WANG Xin, DENG Xiaodong. A numerical study on the circulation and tide in a zigzag bay[J]. Acta Oceanologica Sinica, 2015, 34(1): 119-128. doi: 10.1007/s13131-015-0604-0
Citation: YU Huaming, WANG Zhaohua, KUANG Liang, WANG Lu, BAO Xianwen, WU He, WANG Xin, DENG Xiaodong. A numerical study on the circulation and tide in a zigzag bay[J]. Acta Oceanologica Sinica, 2015, 34(1): 119-128. doi: 10.1007/s13131-015-0604-0

曲折海湾中潮汐和环流的数值研究

doi: 10.1007/s13131-015-0604-0
基金项目: The National Marine Renewable Energy Programs of China under contract Nos GHME2011ZC03, GHME2011Gd01, GHME2012ZC02, GHME2012ZC03, GHME2012ZC05 and GHME2013ZC01; the National Natural Science Foundation of China under contract No. 41406011; the doctoral Fund of Ministry of Education of China under contract No. 20120132120016; the Shandong Province Natural Science Foundation of China under contract No. ZR2012dQ008; the Strategic Priority Research Program of the Chinese Academy of Sciences under contract No. XdA11010201; the Open Laboratory Fund of North China Sea Branch of State Oceanic Administration under contract No. 2012012; the Fundamental Research Funds for the Central Universities under contract No. 201262004; the Public Science and Technology Research Funds Projects of Ocean under contract No. 201305030.

A numerical study on the circulation and tide in a zigzag bay

  • 摘要: 沙埕港是中国东南沿海最复杂的海湾之一, 基于其复杂的地形及水动力过程, 在水动力特征模拟方面极具挑战性. 本文采用最为先进的有限体积海岸海洋模型(FVCOM)来模拟此海区的水动力系统, 对其潮流、潮致余流和水交换过程进行了定量分析. 模型模拟得到的水位和流速均与实测数据具有良好的一致性, 其中, M2分潮与S2分潮振幅的标准差分别为3.66%和4.67%, 最大潮流流速与流向的平均误差分别为10 cm/s和8°. 误差均在允许范围之内, 说明模型是稳定可靠的. 结果显示, 岬角效应对本海区的水动力系统有重大的影响. 水交换过程的模拟表明整个海湾的水交换周期为53天. 本文可反映沙埕港海域的水动力过程, 并为其他研究学者提供可靠有效的科研信息.
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出版历程
  • 收稿日期:  2014-01-21
  • 修回日期:  2014-05-23

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