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Hydrological simulation and uncertainty analysis using the improved TOPMODEL in the arid Manas River basin China

机译:改进的TOPMODEL在干旱的玛纳斯河流域的水文模拟和不确定性分析

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摘要

Understanding the mechanism of complicated hydrological processes is important for sustainable management of water resources in an arid area. This paper carried out the simulations of water movement for the Manas River Basin (MRB) using the improved semi-distributed Topographic hydrologic model (TOPMODEL) with a snowmelt model and topographic index algorithm. A new algorithm is proposed to calculate the curve of topographic index using internal tangent circle on a conical surface. Based on the traditional model, the improved indicator of temperature considered solar radiation is used to calculate the amount of snowmelt. The uncertainty of parameters for the TOPMODEL model was analyzed using the generalized likelihood uncertainty estimation (GLUE) method. The proposed model shows that the distribution of the topographic index is concentrated in high mountains, and the accuracy of runoff simulation has certain enhancement by considering radiation. Our results revealed that the performance of the improved TOPMODEL is acceptable and comparable to runoff simulation in the MRB. The uncertainty of the simulations resulted from the parameters and structures of model, climatic and anthropogenic factors. This study is expected to serve as a valuable complement for widely application of TOPMODEL and identify the mechanism of hydrological processes in arid area.
机译:理解复杂的水文过程的机制对于干旱地区水资源的可持续管理非常重要。本文利用改进的半分布式地形水文模型(TOPMODEL),融雪模型和地形指数算法对玛纳斯河流域(MRB)的水运动进行了模拟。提出了一种利用圆锥形表面上的内切圆计算地形指数曲线的新算法。在传统模型的基础上,使用考虑到太阳辐射的温度改进指标来计算融雪量。使用广义似然不确定性估计(GLUE)方法分析了TOPMODEL模型参数的不确定性。提出的模型表明,地形指数的分布集中在高山上,考虑到辐射,径流模拟的精度有一定提高。我们的结果表明,改进的TOPMODEL的性能可以接受,并且可以与MRB中的径流模拟相媲美。模拟的不确定性来自模型的参数和结构,气候和人为因素。这项研究有望为TOPMODEL的广泛应用提供有价值的补充,并确定干旱地区的水文过程机理。

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