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Influence of bathymetry evolution on position of tidal shear front and hydrodynamic characteristics around the Yellow River estuary

机译:等深线演变对黄河口附近潮汐切变锋位置和水动力特性的影响

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A three dimensional numerical model based on the hydrodynamic module of finite-volume coastal ocean (FVCOM) was established for the Yellow River estuary. The model has been calibrated by observed data and proved to be suitable to reflect the hydrodynamic force in the research area. We employed the model to simulate the tidal shear front off the Yellow River estuary and analyzed the formation, spread and duration of two different types of shear front. To examine the effect of bathymetry evolution on the position of tidal shear front, subaqueous bathymetry of the Yellow River estuary was changed according to the changing patterns obtained from the past few years. Tidal shear front was modeled on both the original and the changed bathymetry. The results show that the position of shear front moved from a shallow to a deep area due to the deposition of bathymetry. The influence of bathymetry evolution on hydrodynamic characteristics including the distribution of salinity and the movement of particles was studied. We found the dispersion areas of low salinity became larger after changing bathymetry and the particles on the surface, middle and bottom layer are able to move further both north and west of Laizhou Bay on the changed bathymetry.
机译:针对黄河口,建立了基于有限体积沿海海洋流体动力模块的三维数值模型。该模型已通过观测数据进行了校准,并被证明适合反映研究区域的水动力。我们利用该模型模拟了黄河口外的潮汐剪切锋,并分析了两种不同类型的剪切锋的形成,传播和持续时间。为了检查测深法对潮汐剪切锋位置的影响,黄河口水下测深法根据过去几年的变化模式进行了改变。潮汐剪切锋以原始和更改后的测深图为模型。结果表明,由于测深仪的沉积,剪切前锋的位置从浅处移至深处。研究了等深线演变对水动力特性(包括盐度分布和颗粒运动)的影响。我们发现,改变测深法后,低盐度的分散区域变得更大,并且在改变的测深法下,表层,中层和底层的颗粒都能够进一步向北和向西移动。

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