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Flood hazard mapping using synthesis hydraulic and geomorphic properties at watershed scale

机译:在流域尺度上利用综合水力和地貌特性绘制洪水灾害图

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摘要

The occurrence of natural phenomena such as floods has caused serious consequences for human societies. The simulation of flood hazard maps and its depth in a river is one of the most complex processes in hydrology. In fact both geomorphological and hydraulic procedures for deriving the flood hazard maps and depth are imperfect at watershed scale. In this study, a combination of both procedures, using a probabilistic approach is used. Flood inundation maps for 2-, 10-, 25-,50- and 100-return period floods using flood routine within HEC-RAS in combination of Arc-GIS and topographic wetness index (TWI) map were produced. TWI threshold was identified using a maximum likelihood method in order to produce flood prone areas and calibrated over the reach of Zirab City. The correlation between TWI threshold and the flood depth was carried out and simple linear regression developed for various return periods. The resulting regression model is used in order to create flood hazard maps with various return periods at watershed scale.
机译:洪水等自然现象的发生给人类社会带来了严重的后果。模拟洪水灾害图及其在河流中的深度是水文学中最复杂的过程之一。实际上,用于得出洪水灾害图和深度的地貌和水力程序在分水岭规模上都是不完善的。在这项研究中,使用概率方法将两种方法结合起来使用。结合Arc-GIS和地形湿度指数(TWI)地图,使用HEC-RAS中的洪水常规,制作了2、10、25、50和100回水期洪水淹没图。使用最大似然法确定TWI阈值,以产生易发洪水的地区,并在Zirab市范围内进行校准。进行了TWI阈值与洪水深度之间的相关性,并针对各种返回期开发了简单的线性回归。使用所得的回归模型来创建在分水岭范围内具有各种返回期的洪水灾害图。

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