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Geospatially based distributed rainfall-runoff modelling for simulation of internal and outlet responses in a semi-forested lower Himalayan watershed

机译:基于地理空间的分布式降雨-径流模型,用于模拟喜马拉雅山下半森林流域的内部和出口响应

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This study presents a Geographic Information System (GIS)-based distributed rainfall-runoff model for simulating surface flows in small to large watersheds during isolated storm events. The model takes into account the amount of interception storage to be filled using a modified Merriam (1960) approach before estimating infiltration by the Smith and Parlange (1978) method. The mechanics of overland and channel flow are modelled by the kinematic wave approximation of the Saint Venant equations which are then numerically solved by the weighted four-point implicit finite difference method. In this modelling the watershed was discretized into overland planes and channels using the algorithms proposed by Garbrecht and Martz (1999). The model code was first validated by comparing the model output with an analytical solution for a hypothetical plane. Then the model was tested in a medium-sized semi-forested watershed of Pathri Rao located in the Shivalik ranges of the Garhwal Himalayas, India. Initially, a local sensitivity analysis was performed to identify the parameters to which the model outputs like runoff volume, peak flow and time to peak flow are sensitive. Before going for model validation, calibration was performed using the Ordered-Physics-based Parameter Adjustment (OPPA) method. The proposed Physically Based Distributed (PBD) model was then evaluated both at the watershed outlet as well as at the internal gauging station, making this study a first of its kind in Indian watersheds. The results of performance evaluation indicate that the model has simulated the runoff hydrographs reasonably well within the watershed as well as at the watershed outlet with the same set of calibrated parameters. The model also simulates, realistically, the temporal variation of the spatial distribution of runoff over the watershed and the same has been illustrated graphically. Copyright © 2011 John Wiley & Sons, Ltd.
机译:这项研究提出了一种基于地理信息系统(GIS)的分布式降雨-径流模型,用于模拟孤立风暴事件期间小到大流域的地表流。该模型考虑了使用改良的Merriam(1960)方法填充的拦截存储量,然后用Smith和Parlange(1978)方法估计渗透率。通过Saint Venant方程的运动波逼近对陆路和河道的力学进行建模,然后通过加权四点隐式有限差分法对其进行数值求解。在该模型中,使用Garbrecht和Martz(1999)提出的算法将分水岭离散为陆平面和河道。首先通过将模型输出与假设平面的解析解进行比较来验证模型代码。然后在印度Garhwal喜马拉雅山Shivalik山脉的Pathri Rao中型半森林分水岭上对该模型进行了测试。最初,进行了局部敏感性分析,以识别模型输出的参数,如径流量,峰流量和峰流量时间是敏感的。在进行模型验证之前,使用基于有序物理的参数调整(OPPA)方法执行校准。然后,在流域出口和内部测量站对拟议的基于物理的分布式(PBD)模型进行了评估,这使该研究成为印度流域中的首例此类研究。性能评估的结果表明,该模型在流域内以及流域出口处使用相同的校准参数对流域水文图进行了较好的模拟。该模型还现实地模拟了流域上径流的空间分布的时间变化,并且已通过图形方式对其进行了说明。版权所有©2011 John Wiley&Sons,Ltd.

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