Assessing the non-stationarity of low flows and their scale-dependent relationships with climate and human forcing

被引:23
作者
Liu, Saiyan [1 ]
Huang, Shengzhi [1 ]
Xie, Yangyang [2 ]
Huang, Qiang [1 ]
Wang, Hao [3 ]
Leng, Guoyong [4 ,5 ]
机构
[1] Xian Univ Technol, State Key Lab Ecohydraul Northwest Arid Reg China, Xian 710048, Shaanxi, Peoples R China
[2] Yangzhou Univ, Modern Rural Water Resources Res Inst, Sch Hydrol Energy & Power Engn, Yangzhou 225009, Jiangsu, Peoples R China
[3] China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China
[4] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
[5] Univ Oxford, Environm Change Inst, Oxford OX1 3QY, England
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Low flow; Non-stationarity; Change point; Discrete wavelet transform; Scale-dependent relationship; SPATIAL-TEMPORAL CHANGES; CHINA CHANGING PATTERNS; UNGAUGED SITES; LOESS PLATEAU; RIVER-BASIN; TRENDS; STREAMFLOW; NONSTATIONARITY; PRECIPITATION; DERIVATION;
D O I
10.1016/j.scitotenv.2019.06.025
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
It is necessary to assess the non-stationarity of a hydrological series under changing environments. This study aimed to determine the validity of the stationarity of low flow series in terms of trends and possible change points, as well as the time-scale that is responsible for the production of trends and change points in low flow series. Further, we investigated how climatic variables affect low flow variations by studying their scale-dependent relationships. The modified Mann-Kendall trend test, heuristic segmentation method, discrete wavelet transform, and Pearson correlation coefficient were co-utilized to achieve these objectives. The Wei River Basin (WRB), a typical Loess Plateau region in China, was selected as the case study. Results showed significantly decreasing trends and change points in the low flow series, indicating that its stationarity assumption is invalid. The 2-year and 4-year events were the most important time-scales contributing to the trend of the original low flow series, and the 8-year periodic scale was the most influential frequency component for change point generation. Additionally, the strongest scale-dependent relationships among high frequency components (2-year and 4-year scales) of the low flow series and climatic variables (precipitation, potential evaporation, and soil moisture) demonstrated the importance of climatic factors for driving the trends of a low flow series. In contrast, human activities, including water withdrawals and water and soil conservation projects showed strong influences on the non-stationarity of low flows via affecting the low frequency component (8-year frequency and approximate components). These findings contribute to a better understanding temporal variations of low flow and their responses to changing environments, and the results also would be helpful for local water resources management as well as agricultural and ecological sustainable development. (C) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页码:244 / 256
页数:13
相关论文
共 51 条
[1]   Scale invariance in the nonstationarity of human heart rate -: art. no. 168105 [J].
Bernaola-Galván, P ;
Ivanov, PC ;
Amaral, LAN ;
Stanley, HE .
PHYSICAL REVIEW LETTERS, 2001, 87 (16) :1-168105
[2]   Impact of climate change and human activities on runoff in the Weihe River Basin, China [J].
Chang, Jianxia ;
Wang, Yimin ;
Istanbulluoglu, Erkan ;
Bai, Tao ;
Huang, Qiang ;
Yang, Dawen ;
Huang, Shengzhi .
QUATERNARY INTERNATIONAL, 2015, 380 :169-179
[3]   Regional analysis of low flow using L-moments for Dongjiang basin, South China [J].
Chen, Yongqin David ;
Huang, Guoru ;
Shao, Quanxi ;
Xu, Chong-Yu .
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 2006, 51 (06) :1051-1064
[4]   Probabilistic assessment of remote sensing-based terrestrial vegetation vulnerability to drought stress of the Loess Plateau in China [J].
Fang, Wei ;
Huang, Shengzhi ;
Huang, Qiang ;
Huang, Guohe ;
Wang, Hao ;
Leng, Guoyong ;
Wang, Lu ;
Guo, Yi .
REMOTE SENSING OF ENVIRONMENT, 2019, 232
[5]   Examining the applicability of different sampling techniques in the development of decomposition-based streamflow forecasting models [J].
Fang, Wei ;
Huang, Shengzhi ;
Ren, Kun ;
Huang, Qiang ;
Huang, Guohe ;
Cheng, Guanhui ;
Li, Kailong .
JOURNAL OF HYDROLOGY, 2019, 568 :534-550
[6]   Copulas-based risk analysis for inter-seasonal combinations of wet and dry conditions under a changing climate [J].
Fang, Wei ;
Huang, Shengzhi ;
Huang, Guohe ;
Huang, Qiang ;
Wang, Hao ;
Wang, Lu ;
Zhang, Ying ;
Li, Pei ;
Ma, Lan .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2019, 39 (04) :2005-2021
[7]   Evolution of low flows in the Czech Republic [J].
Fiala, Theodor ;
Ouarda, Taha B. M. J. ;
Hladny, Josef .
JOURNAL OF HYDROLOGY, 2010, 393 (3-4) :206-218
[8]  
Giuntoli I, 2013, J HYDROL, V482, P105, DOI [10.1016/j.jhydrol.2012.12.038, 1]
[9]   Statistics of low flow: Theoretical derivation of the distribution of minimum streamflow series [J].
Gottschalk, Lars ;
Yu, Kun-xia ;
Leblois, Etienne ;
Xiong, Lihua .
JOURNAL OF HYDROLOGY, 2013, 481 :204-219
[10]   A method for low-flow estimation at ungauged sites: a case study in Wallonia (Belgium) [J].
Grandry, M. ;
Gailliez, S. ;
Sohier, C. ;
Verstraete, A. ;
Degre, A. .
HYDROLOGY AND EARTH SYSTEM SCIENCES, 2013, 17 (04) :1319-1330