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利用改进的 TOPMODEL 对中国干旱玛纳斯河流域进行水文模拟和不确定性分析。

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

机构信息

Hydrology and Water Resources College, Hohai University, Nanjing, 210098, P. R. China.

Shihezi University, Shihezi, 832003, P. R. China.

出版信息

Sci Rep. 2018 Jan 11;8(1):452. doi: 10.1038/s41598-017-18982-8.

Abstract

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.

摘要

理解复杂水文过程的机制对于干旱地区水资源的可持续管理至关重要。本研究采用改进的具有融雪模型和地形指数算法的半分布式地形水文模型(TOPMODEL)对玛纳斯河流域(MRB)的水运动进行了模拟。提出了一种新的算法,使用圆锥面上的内接正切圆来计算地形指数曲线。基于传统模型,使用考虑太阳辐射的改进温度指标来计算融雪量。利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。所提出的模型表明,地形指数的分布集中在高山地区,考虑辐射后,对径流量模拟的准确性有一定的提高。我们的结果表明,改进的 TOPMODEL 的性能是可以接受的,并且可以与 MRB 中的径流量模拟相媲美。模拟的不确定性来自于模型的参数和结构、气候和人为因素。本研究有望为 TOPMODEL 的广泛应用提供有价值的补充,并确定干旱地区水文过程的机制。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c18f/5765026/9547c9aa6f1d/41598_2017_18982_Fig1_HTML.jpg

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