Flood-tide interaction numerical simulation at Min River tidal reach

Cifu Fu , Qiuxing Liu , Fujiang Yu , Jianxi Dong
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引用次数: 3

Abstract

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.

岷江潮汐段涨潮相互作用数值模拟
本文分析了闽江潮汐段的洪潮特征,利用闽江河口关键区域的高分辨率GIS数据,建立了网格分辨率最高为50-100m的高分辨率洪潮耦合模型。模型采用非结构化三角网格,关键区域网格分辨率可达50-100m。选择朱齐河段作为洪水边界,对2006年6月6日的洪水过程进行了3次数值模拟试验。实验结果表明,与仅考虑洪潮和洪潮的模型结果相比,各验潮仪的模拟结果与实测数据吻合较好,且在洪潮信号到达的岷江不同河段,原有的潮汐特征发生了变化。文山里站、解放桥站洪水特征明显,仙安站、白岩滩站、官头站洪潮混合特征明显。在南海峡咸南至关头的河道中,由于水流速度在高潮时减小而在低潮时增大,潮洪相互作用强。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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