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Flood-tide interaction numerical simulation at Min River tidal reach

机译:闽江潮汐段洪潮相互作用数值模拟

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Flood and tide features atMin River tidal reach are analyzed anda high-resolution flood-tide coupled model which useshigh-resolution GIS data for Minjiang Estuary with the highest grid resolution of 50-100m at key areas isestablished in this paper. Unstructured triangular mesh that can realize the grid resolution of 50-100m at key areas is employed in the model. Zhuqi section is chosen for flood boundary, and three numerical experimentsare conducted for June 6 2006 flood process. The experimental results indicate that, when coupled with tide and flood, the simulation of each tide gauge agrees very well with measured data compared withmodelresults only with flood or tide, and the original tidal features are changedat the different sections in Min River tidal reachedby the flood signals. Obvious flood characteristics are shown in Wenshanli and Jiefang Bridge station and flood-tidal mixed characteristics are shown in Xianan, Baiyantan and Guantou station.The strong interaction between tide and floodoccursin the watercourse (from Xiannan in South Channel to Guantou) because the current velocity is reduced during high water time but increasedduringlow water time.
机译:分析了闽江潮汐段的潮汐潮汐特征,建立了高分辨率的潮汐耦合模型,该模型利用高分辨率GIS数据为Min江河口提供了关键区域的最高网格分辨率为50-100m。该模型采用非结构化三角网格,可以在关键区域实现50-100m的网格分辨率。选择朱岐断面作为洪水边界,并对2006年6月6日的洪水过程进行了三个数值试验。实验结果表明,与潮汐和洪水相结合时,与仅洪水或潮汐的模型结果相比,每个潮汐计的模拟结果与实测数据吻合得很好,并且洪水在Min河潮汐的不同断面改变了原始潮汐特征。信号。文山里和解放桥站表现出明显的洪水特征,咸安,白岩滩和关头站表现出洪潮混合特征。潮汐与洪水在水道(从南通道的仙南到关头)之间发生了强烈的相互作用。高水时间减少,但低水时间增加。

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