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A numerical study on the effect of tidal flat's slope on tidal dynamics in the Xiangshan Bay, China

机译:象山湾潮滩坡度对潮汐动力学影响的数值研究

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摘要

The Xiangshan Bay is a semi-enclosed and narrow bay, which is characterized by large scale tidal flats and has been historically utilized through coastal construction and aquaculture engineering. The hydrodynamic model using the Finite Volume Coastal Ocean Model (FVCOM) was constructed to examine the changes of tidal dynamics due to the variation of tidal flat slopes. According to the model results, a decreased slope of a tidal flat would amplify the M2 tidal amplitude and delay the M2 tidal phase in the inner harbor, due to an increased tidal prism, and vice versa. The amplitude of the main shallow-water tide M4 would be amplified/dampened in the entire bay due to the changed bottom friction, if the tidal flat's slope were reduced/increased at the Tie inlet. The phase was advanced. The change of a tidal flat's slope at the Tie inlet had greater impacts on tidal amplitude, phase and duration asymmetry, than that at the Xihu inlet. The impact of changes of the tidal flat slope at the Xihu inlet was small and was constrained locally. Changes in the tidal flats' slopes at the Tie and Xihu inlets changed the tidal duration asymmetry, residual current and tidal energy via modulating tides. The ebb dominance decreased when the tidal flat's slope at the Tie inlet was changed. Decreased/increased ebb dominance occurred when the tidal flat's slope was reduced/increased at the Xihu inlet. The residual current and tidal energy density was amplified/dampened and more/less tidal energy was dissipated, with reduced/increased slope at both of the inlets. The findings in this study are instructive to coastal engineering and estuarine management.
机译:象山湾是一个半封闭,狭窄的海湾,具有大规模的滩涂特征,历史上一直通过沿海建设和水产养殖工程加以利用。建立了使用有限体积沿海海洋模型(FVCOM)的流体动力学模型,以研究由于潮汐平缓坡度的变化而引起的潮汐动力学变化。根据模型结果,由于增加的潮汐棱镜,减小的潮汐坡度将放大内港的M2潮汐振幅并延迟M2潮汐相位,反之亦然。如果潮汐平面的斜度在领带进口处减小/增加,则由于底部摩擦力的变化,整个浅水湾的主要浅水潮M4的振幅将被放大/减弱。该阶段已进行。与西湖进口相比,铁带进口处的滩涂坡度变化对潮汐幅度,相位和持续时间的不对称性影响更大。西湖入海口滩涂坡度变化的影响很小,受到局部限制。铁和西湖进口处滩涂坡度的变化通过调节潮汐改变了潮汐持续时间的不对称性,剩余电流和潮汐能。当铁带进口处的潮滩坡度发生变化时,起伏优势下降。当西湖入海口的潮滩坡度减小/增大时,退潮优势减小/增大。剩余电流和潮汐能密度被放大/衰减,潮汐能被消散/消散,两个入口处的斜率减小/增大。这项研究的发现对沿海工程和河口管理具有指导意义。

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  • 来源
    《海洋学报(英文版)》 |2018年第9期|29-40|共12页
  • 作者单位

    Ocean College, Zhejiang University, Zhoushan 316021, China;

    State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310058, China;

    Ocean College, Zhejiang University, Zhoushan 316021, China;

    Ocean College, Zhejiang University, Zhoushan 316021, China;

    State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310058, China;

    Ocean College, Zhejiang University, Zhoushan 316021, China;

    State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310058, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-19 03:57:49
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