首页> 外文期刊>Journal of The Institution of Engineers (India) >Flow Routing and Surface Water Balance Simulation of a Tank Cascaded Catchment Using Coupled MIKE SHE/MIKE 11 Modeling
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Flow Routing and Surface Water Balance Simulation of a Tank Cascaded Catchment Using Coupled MIKE SHE/MIKE 11 Modeling

机译:基于MIKE SHE / MIKE 11耦合模型的坦克梯级流域水流路径和地表水平衡模拟

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Hydrology of a tank cascaded basin in semiarid region is unique and different from a plain terrain hydrology as it consists of intervening surface storage structures called tanks. The incorporation of physical processes of irrigation tank cascaded system in hydrological modeling is essential for accurate estimation and simulation of its water balance components. The earlier studies of rainfall-runoff modeling in such catchments and the effects and processes of these tanks were lumped while modeling as it requires extensive data. Routing through the streams without considering the intervening tank storages will not give accurate estimation of surface water resource potential. Hence, an attempt has been made in this study to characterize the physical processes and to simulate the flow routing through an irrigation tank cascaded system with the application of coupled MIKE SHE and MIKE 11, a fully integrated physically based deterministic and distributed model. With the help of primary and secondary data, the model has been set up by coupling MIKE SHE and MIKE 11 model and the dynamics of water movement has been simulated. The model simulation results have been evaluated through calibration and validation of simulated tank yield with that of observed values. Water level at three tank outlets located at the upper, middle and tail reach of the tank cascaded catchment was used to study the model performance evaluation. The Nash-Sutcliffe coefficients obtained are 0.91, 0.94 and 0.92 for three tank water levels showing satisfactory goodness of fit between the observed and simulated water levels. The statistical parameters obtained from the validation process, such as error matrix, correlation coefficient and Nash-Sutcliffe coefficient values, indicate good simulation and prediction capability of the developed coupled model that incorporates a methodology which takes into account all the physical processes of the tank cascaded system.
机译:半干旱地区的水库级联盆地的水文学是独特的,与平原地形水文学不同,因为它由称为水箱的中间表面存储结构组成。在水文模型中纳入灌溉水箱级联系统的物理过程对于准确估算和模拟其水平衡分量至关重要。由于需要大量数据,因此在此类流域中对降雨径流模型以及这些水箱的影响和过程的早期研究被集中在一起。在不考虑中间水箱存储的情况下穿过河流的路线将无法准确估算地表水资源潜力。因此,在这项研究中,人们试图结合耦合的MIKE SHE和MIKE 11(一个完全基于物理的确定性和分布式模型)的应用来表征物理过程并模拟通过灌溉水箱级联系统的水流路径。借助于主要和辅助数据,通过将MIKE SHE和MIKE 11模型耦合建立了模型,并模拟了水​​运动的动力学。通过对模拟储罐的观测值进行校准和验证,对模型模拟结果进行了评估。使用位于水箱级联流域上部,中部和尾部的三个水箱出口处的水位来研究模型性能评估。对于三个水箱水位,获得的Nash-Sutcliffe系数分别为0.91、0.94和0.92,显示了在观察到的水位与模拟水位之间令人满意的拟合度。从验证过程中获得的统计参数,例如误差矩阵,相关系数和Nash-Sutcliffe系数值,表明已开发的耦合模型具有良好的仿真和预测能力,该模型结合了一种方法,该方法考虑了级联储罐的所有物理过程系统。

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