摘要
The Yellow River is the second largest river in China,and it is of paramount importance as it serves various hydro-ecological functions for its inhabitants and environment.It consumes 12%of the water in China,with annual runoff accounting for 2%of the whole country.For sustainable water resources management under climate change and land cover changes(mainly the vegetation change),it is essential to understand the terrestrial water storage change(WSC)and its major driving factors in the Yellow River Basin(YRB)[1].
作者
Congcong Li
Yongqiang Zhang
Yanjun Shen
Qiang Yu
李聪聪;张永强;沈彦俊;于强(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 Resources and Environmental Science,Hebei Normal University,Shijiazhuang 050024,China;Center for Agricultural Resources Research,Institute of Genetics and Developmental Biology,Chinese Academy of Sciences,Shijiazhuang 050021,China;State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau,Northwest A&F University,Yangling 712100,China)
基金
supported by Pioneer Talents Program of Chinese Academy of Sciences and the National Natural Science Foundation of China(41971032)。
