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2D Unsteady Flow Routing and Flood Inundation Mapping for Lower Region of Brazos River Watershed

机译:布拉索斯河流域下游地区的二维非定常流动路径与洪水淹没制图

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Present study uses two dimensional flow routing capabilities of hydrologic engineering center's river analysis system (HEC-RAS) for flood inundation mapping in lower region of Brazo River watershed subjected to frequent flooding. For analysis, river reach length of 20 km located at Richmond, Texas, was considered. Detailed underlying terrain information available from digital elevation model of 1/9-arc second resolution was used to generate the two-dimensional (2D) flow area and flow geometries. Streamflow data available from gauging station USGS08114000 was used for the full unsteady flow hydraulic modeling along the reach. Developed hydraulic model was then calibrated based on the manning's roughness coefficient for the river reach by comparison with the downstream rating curve. Corresponding water surface elevation and velocity distribution obtained after 2D hydraulic simulation were used to determine the extent of flooding. For this, RAS mapper's capabilities of inundation mapping in HEC-RAS itself were used. Mapping of the flooded areas based on inflow hydrograph on each time step were done in RAS mapper, which provided the spatial distribution of flow. The results from this study can be used for flood management as well as for making land use and infrastructure development decisions.
机译:本研究使用水文工程中心的河流分析系统(HEC-RAS)的二维流路由功能,对频繁洪水的布拉索河流域下游地区的洪水泛滥进行制图。为了进行分析,考虑了位于得克萨斯州里士满的20公里河段。可从1/9弧秒分辨率的数字高程模型获得的详细基础地形信息用于生成二维(2D)流动面积和流动几何形状。测量站USGS08114000提供的流量数据用于沿河段的全非恒定流水力建模。然后,根据曼宁的河道糙率系数与下游的额定曲线进行比较,对开发的水力模型进行校准。二维水力模拟后获得的相应水面高程和速度分布用于确定淹没程度。为此,使用了HEC-RAS本身中的RAS映射器的淹没映射功能。在RAS映射器中基于每个时间步的流入水文图对洪水区域进行了映射,从而提供了流量的空间分布。这项研究的结果可用于洪水管理以及制定土地使用和基础设施开发决策。

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