Impacts of Climate Change on Runoff in the Heihe River Basin, China

被引:5
作者
Liu, Qin [1 ,2 ]
Cheng, Peng [2 ]
Lyu, Meixia [2 ]
Yan, Xinyang [2 ]
Xiao, Qingping [3 ]
Li, Xiaoqin [2 ]
Wang, Lei [4 ]
Bao, Lili [2 ]
机构
[1] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 730000, Peoples R China
[2] Meteorol Serv Ctr Gansu Prov, Lanzhou 730020, Peoples R China
[3] Gongnongqu Elect Pumping Stn, Lanzhou 730020, Peoples R China
[4] CMA Earth Syst Modeling & Predict Ctr, Beijing 100081, Peoples R China
关键词
Heihe River Basin; climate change; runoff changes; machine learning methods; runoff forecasting models; PRECIPITATION; EVAPOTRANSPIRATION;
D O I
10.3390/atmos15050516
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Located in the central part of the arid regions of Northwest China, the Heihe River Basin (HRB) plays an important role in wind prevention, sand fixation, and soil and water conservation as the second largest inland river basin. In the context of the warming and wetting climate observed in Northwest China, the situation of the ecological environment in the HRB is of significant concern. Using the data from meteorological observation stations, grid fusion and hydrological monitoring, this study analyzes the multi-scale climate changes in the HRB and their impacts on runoff. In addition, predictive models for runoff in the upper and middle reaches were developed using machine learning methods. The results indicate that the climate in the HRB has experienced an overall warming and wetting trend over the past 60 years. At the same time, there are clear regional variabilities in the climate changes. Precipitation shows decreasing trends in the northwestern part of the HRB, while it shows increases at rates higher than the regional average in the southeastern part. Moreover, the temperature increases are generally smaller in the upper reaches than those in the middle and lower reaches. Over the past 60 years, there has been a remarkable increase in runoff at the Yingluo Gorge (YL) hydrological station, which exhibits a distinct "single-peak" pattern in the variation of monthly runoff. The annual runoff volume at the YL (ZY) hydrological station is significantly correlated with the precipitation in the upper (middle) reaches, indicating the precipitation is the primary influencing factor determining the annual runoff. Temperature has a significant impact only on the runoff in the upper reaches, while its impact is not significant in the middle reaches. The models trained by the support vector machines and random forest models perform best in predicting the annual runoff and monthly runoff, respectively. This study can provide a scientific basis for environmental protection and sustainable development in the HRB.
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页数:15
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