Identifying how future climate and land use/cover changes impact streamflow in Xinanjiang Basin, East China

被引:83
作者
Guo, Yuxue [1 ]
Fang, Guohua [2 ]
Xu, Yue-Ping [1 ]
Tian, Xin [3 ]
Xie, Jingkai [1 ]
机构
[1] Zhejiang Univ, Inst Hydrol & Water Resources Civil Engn & Archit, Hangzhou 310058, Peoples R China
[2] Hohai Univ, Coll Water Conservancy & Hydropower Engn, Nanjing 210098, Peoples R China
[3] Delft Univ Technol, Fac Civil Engn & Geosci, Dept Water Management, NL-2623 CN Delft, Netherlands
关键词
Multiple scenarios; Climate change; Land use/cover change; Streamflow response; Uncertainty; Attribution; RIVER-BASIN; RUNOFF PROJECTIONS; USE/LAND COVER; WATER-QUALITY; CA-MARKOV; MODEL; URBANIZATION; CATCHMENT; UNCERTAINTY; HYDROLOGY;
D O I
10.1016/j.scitotenv.2019.136275
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Climate and land use/cover changes are the main factors altering hydrological regimes. To understand the impacts of climate and land use/cover changes on streamflow within a specific catchment, it is essential to accurately quantify their changes given many possibilities. We propose an integrated framework to assess how individual and combined climate and land use/cover changes impact the streamflow of Xinanjiang Basin, in East China, in the future. Five bias-corrected and downscaled General Circulation Model (GCM) projections are used to indicate the inter-model uncertainties under three Representative Concentration Pathways (RCPs). Additionally, three land use/cover change scenarios representing a range of tradeoffs between ecological protection (EP) and urban development (UD) are projected by Cellular Automata - Markov (CA-Markov). The streamflow in 2021-2050 is then assessed using the calibrated Soil and Water Assessment Tool (SWAT) with 15 scenarios and 75 possibilities. Finally, the uncertainty and attribution of streamflow changes to climate and land use/cover changes at monthly and annual scale are analyzed. Results show that while both land use/cover change alone and combined changes project an increase in streamflow, there is a disagreement on the direction of streamflow change under climate change alone. Future streamflow may undergo a more blurred boundary between the flood and non-flood seasons, potentially easing the operation stress of Xinanjiang Reservoir for water supply or hydropower generation. We find that the impacts of climate and land use/cover changes on monthly mean streamflow are sensitive to the impermeable area (IA).The impacts of climate change are stronger than those induced by land use/cover change under EP (i.e., lower IA); and land use/cover change has a greater impact in case of UD (i.e., higher IA). However, changes in annual mean streamfiow are mainly driven by land use/cover change, and climate change may decrease the influence attributed to land use/cover change. (C) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页数:13
相关论文
共 68 条
[1]  
Abbaspour KC, 2007, MODSIM 2007: INTERNATIONAL CONGRESS ON MODELLING AND SIMULATION, P1603
[2]   Understanding climate and land surface changes impact on water resources using Budyko framework and remote sensing data in Ethiopia [J].
Abera, Wuletawu ;
Tamene, Lulseged ;
Abegaz, Assefa ;
Solomon, Dawit .
JOURNAL OF ARID ENVIRONMENTS, 2019, 167 :56-64
[3]   Quantifying the relative impact of climate and human activities on streamflow [J].
Ahn, Kuk-Hyun ;
Merwade, Venkatesh .
JOURNAL OF HYDROLOGY, 2014, 515 :257-266
[4]   Modelling the effects of land use and climate changes on hydrology in the Ursern Valley, Switzerland [J].
Alaoui, A. ;
Willimann, E. ;
Jasper, K. ;
Felder, G. ;
Herger, F. ;
Magnusson, J. ;
Weingartner, R. .
HYDROLOGICAL PROCESSES, 2014, 28 (10) :3602-3614
[5]   Prediction of land use changes based on Land Change Modeler and attribution of changes in the water balance of Ganga basin to land use change using the SWAT model [J].
Anand, Jatin ;
Gosain, A. K. ;
Khosa, R. .
SCIENCE OF THE TOTAL ENVIRONMENT, 2018, 644 :503-519
[6]  
[Anonymous], INT C COMP COMM TECH
[7]   Large area hydrologic modeling and assessment - Part 1: Model development [J].
Arnold, JG ;
Srinivasan, R ;
Muttiah, RS ;
Williams, JR .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 1998, 34 (01) :73-89
[8]   Modelling and analyzing the watershed dynamics using Cellular Automata (CA)-Markov model - A geo-information based approach [J].
Behera, Mukunda D. ;
Borate, Santosh N. ;
Panda, Sudhindra N. ;
Behera, Priti R. ;
Roy, Partha S. .
JOURNAL OF EARTH SYSTEM SCIENCE, 2012, 121 (04) :1011-1024
[9]   Hydrological responses to land use/land cover change and climate variability in contrasting agro-ecological environments of the Upper Blue Nile basin, Ethiopia [J].
Berihun, Mulatu Liyew ;
Tsunekawa, Atsushi ;
Haregeweyn, Nigussie ;
Meshesha, Derege Tsegaye ;
Adgo, Enyew ;
Tsubo, Mitsuru ;
Masunaga, Tsugiyuki ;
Fenta, Ayele Almaw ;
Sultan, Dagnenet ;
Yibeltal, Mesenbet ;
Ebabu, Kindiye .
SCIENCE OF THE TOTAL ENVIRONMENT, 2019, 689 :347-365
[10]   Evaluation and application of a SWAT model to assess the climate change impact on the hydrology of the Himalayan River Basin [J].
Bhatta, Binod ;
Shrestha, Sangam ;
Shrestha, Pallav K. ;
Talchabhadel, Rocky .
CATENA, 2019, 181