摘要
国家社会经济的可持续发展与可用淡水资源量关系密切.我国人口众多,水资源供需矛盾较突出.现有的天然河川径流资料缺失率较高,参考站点密度不足,在年际和季节变化尺度上存在较大偏差,难以客观揭示大尺度河川径流变化的自然规律.本研究基于VIC(The Variable Infiltration Capacity)分布式水文模型,结合参数不确定分析、流向校正和统计后处理方法,建立了一套长时序、多站点、高质量的天然河川径流资料.全国330个水文站分别约有83%和56%水文站的NSE值、KGE值大于0.70,该天然径流数据集可以为变化环境下水文过程模拟与水资源综合管理提供重要基础数据与科学服务.
Reconstruction of natural streamflow is fundamental to the sustainable management of water resources.In China,previous reconstructions from sparse and poor-quality gauge measurements have led to large biases in simulation of the interannual and seasonal variability of natural flows.Here we use a well-trained and tested land surface model coupled to a routing model with flow direction correction to reconstruct the first high-quality gauge-based natural streamflow dataset for China,covering all its330 catchments during the period from 1961 to 2018.A stronger positive linear relationship holds between upstream routing cells and drainage areas,after flow direction correction to 330 catchments.We also introduce a parameter-uncertainty analysis framework including sensitivity analysis,optimization,and regionalization,which further minimizes biases between modeled and inferred natural streamflow from natural or near-natural gauges.The resulting behavior of the natural hydrological system is represented properly by the model which achieves high skill metric values of the monthly streamflow,with about 83%of the 330 catchments having Nash-Sutcliffe efficiency coefficient(NSE)>0.7,and about56%of the 330 catchments having Kling-Gupta efficiency coefficient(KGE)>0.7.The proposed construction scheme has important implications for similar simulation studies in other regions,and the developed low bias long-term national datasets by statistical postprocessing should be useful in supporting river management activities in China.
作者
缪驰远
苟娇娇
傅伯杰
汤秋鸿
段青云
陈忠升
雷慧闽
陈杰
郭家力
Alistair G.L.Borthwick
丁文峰
段兴武
李运刚
孔冬贤
郭晓莹
吴京文
Chiyuan Miao;Jiaojiao Gou;Bojie Fu;Qiuhong Tang;Qingyun Duan;Zhongsheng Chen;Huimin Lei;Jie Chen;Jiali Guo;Alistair G.L.Borthwick;Wenfeng Ding;Xingwu Duan;Yungang Li;Dongxian Kong;Xiaoying Guo;Jingwen Wu(State Key Laboratory of Earth Surface Processes and Resource Ecology,Faculty of Geographical Science,Beijing Normal University,Beijing 100875,China;State Key Laboratory of Urban and Regional Ecology,Research Center for Eco-Environmental Sciences,Chinese Academy of Sciences,Beijing 100085,China;Key Laboratory of Water Cycle and Related Land Surface Processes,Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101,China;College of Land and Resources,China West Normal University,Nanchong 637009,China;State Key Laboratory of Hydroscience and Engineering,Department of Hydraulic Engineering,Tsinghua University,Beijing 100084,China;State Key Laboratory of Water Resources and Hydropower Engineering Science,Wuhan University,Wuhan 430072,China;College of Hydraulic and Environmental Engineering,China Three Gorges University,Yichang 443002,China;Engineering Research Center of Eco-environment in Three Gorges Reservoir Region,Ministry of Education,China Three Gorges University,Yichang 443002,China;School of Engineering,the University of Edinburgh,the King’s Buildings,Edinburgh EH93JL,UK;Changjiang River Scientific Research Institute,Wuhan 430010,China;Institute of International Rivers and Eco-security,Yunnan University,Kunming 650091,China)
基金
supported by the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK0405)
the National Natural Science Foundation of China(42041006,41877155)
support from the Center for Geodata and Analysis,Faculty of Geographical Science,Beijing Normal University(https://gda.bnu.edu.cn/)
reviewed by Ministry of Natural Resources of the People’s Republic of China(GS(2021)7303)。