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Projection of future streamflow of the Hunza River Basin,Karakoram Range(Pakistan)using HBV hydrological model

查看全文 作　　者：Ayaz Fateh [1,2]ALI;XIAO Cun-[3]de;ZHANG Xiao-[1,2]peng;Muhammad [1,2]ADNAN;Mudassar [2,4]IQBAL;Garee [5]KHAN 高影响力作者 机构地区：[1]State Key Laboratory of Cryospheric Science,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China;[2]University of Chinese Academy of Sciences,Beijing 100049,China;[3]State Key Laboratory of Land Surface and Resource Ecology,Beijing Normal University,Beejing 100875,China;[4]Key Laboratory of land Surface Process and Climate Change in Cold and Arid Regions,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 73o000,China;[5]Department of Earth Sciences,Karakoram International University,Gilgit 15100,Pakistan高影响力机构 出　　处：《Journal of Mountain Science》索引2018年第15卷第10期,共18页高影响力期刊 基　　金：the National Natural Science foundation of China(Grant Nos.41690145 and 41670158) 摘　　要：Hydrologiska Byrans Vattenbalansavdeling(HBV) Light model was used to evaluate the performance of the model in response to climate change in the snowy and glaciated catchment area of Hunza River Basin. The study aimed to understand the temporal variation of streamflow of Hunza River and its contribution to Indus River System(IRS). HBV model performed fairly well both during calibration(R2=0.87, Reff=0.85, PBIAS=-0.36) and validation(R2=0.86, Reff=0.83, PBIAS=-13.58) periods on daily time scale in the Hunza River Basin. Model performed better on monthly time scale with slightly underestimated low flows period during bothcalibration(R2=0.94, Reff=0.88, PBIAS=0.47) and validation(R2=0.92, Reff=0.85, PBIAS=15.83) periods. Simulated streamflow analysis from 1995-2010 unveiled that the average percentage contribution of snow, rain and glacier melt to the streamflow of Hunza River is about 16.5%, 19.4% and 64% respectively. In addition, the HBV-Light model performance was also evaluated for prediction of future streamflow in the Hunza River using future projected data of three General Circulation Model(GCMs) i.e. BCC-CSM1.1, CanESM2, and MIROCESM under RCP2.6, 4.5 and 8.5 and predictions were made over three time periods, 2010-2039, 2040-2069 and 2070-2099, using 1980-2010 as the control period. Overall projected climate results reveal that temperature and precipitation are the most sensitiveparameters to the streamflow of Hunza River. MIROC-ESM predicted the highest increase in the future streamflow of the Hunza River due to increase in temperature and precipitation under RCP4.5 and 8.5 scenarios from 2010-2099 while predicted slight increase in the streamflow under RCP2.6 during the start and end of the 21 th century. However, BCCCSM1.1 predicted decrease in the streamflow under RCP8.5 due to decrease in temperature and precipitation from 2010-2099. However, Can ESM2 predicted 22%-88% increase in the streamflow under RCP4.5 from 2010-2099. The results of this study could be useful for decision making and effective future strategic plans for water management and their sustainability in the region. 关 键 词：流水量 HBV 流速 巴基斯坦 水文学 模特儿 评估模型 设计
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