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Simulation of '6.10' Storm Flood Using a 2-D Hybrid Approach in Shalan Watershed in Heilongjiang Province

机译:基于二维混合法的黑龙江省沙兰流域“ 6.10”暴雨洪水模拟

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摘要

Using supposed rainfall process of "6.10" storm in Shalan catchment and extracted drainage network from raster DEM with 90-m resolution, a hybrid approach which combining simplified hydrology process with 2-D hydraulic model was developed and used to simulate the storm flash flood in Shalan River basin in Heilongjiang Province. The result shows, the maximum flood discharge in outlet is 415 m~3/s, the maximum water depth nearby the Shalan town is 1.3 m, flash flood lasting period is 5 -6 h, and 1 -2 h for water depth over 1 m at the same location. The flood zone mainly locates along the Shalan River with the width of 500 m. Though default of flood observation and remote sensing data, the simulation shows reasonable agreement with real situation. The results imply that the proposed approach are apt to simulate storm flash flood with reliable resolution in mountainous area or valleys, it can served as a new tool for analysis of national storm flash flood in mountainous area or valleys.
机译:利用莎兰流域假定的“ 6.10”暴雨降雨过程,并从90m分辨率的栅格DEM中提取排水网络,提出了一种简化的水文过程与二维水力模型相结合的混合方法,并用于模拟暴雨洪水。黑龙江省的沙兰河流域。结果表明,出水口最大洪水流量为415 m〜3 / s,沙兰镇附近最大水深为1.3 m,山洪持续时间为5 -6 h,水深大于1时为-1 -2 h。 m在同一位置。洪水带主要分布在沙兰河沿岸,宽度为500 m。尽管洪灾观测和遥感数据没有默认值,但仿真结果与实际情况显示出合理的一致性。结果表明,该方法易于模拟山区或山谷暴雨洪水,具有可靠的分辨率,可作为分析山区或山谷国家暴雨洪水的新工具。

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