Key Laboratory of Soil and Water Conservation on the Loess Plateau, Yellow River Institute of Hydraulic Research, Yellow River Conservancy Commission, Zhengzhou, 450003, China
Henan Key Laboratory of Ecological Environment Protection and
Restoration of the Yellow River Basin, Yellow River Institute of Hydraulic Research, Zhengzhou, 45003, China
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
Daoxi Wang
Key Laboratory of Soil and Water Conservation on the Loess Plateau, Yellow River Institute of Hydraulic Research, Yellow River Conservancy Commission, Zhengzhou, 450003, China
Henan Key Laboratory of Ecological Environment Protection and
Restoration of the Yellow River Basin, Yellow River Institute of Hydraulic Research, Zhengzhou, 45003, China
Peiqing Xiao
Key Laboratory of Soil and Water Conservation on the Loess Plateau, Yellow River Institute of Hydraulic Research, Yellow River Conservancy Commission, Zhengzhou, 450003, China
Runliang Xia
Henan Engineering Research Center of Smart Water Conservancy, Yellow River Institute of Hydraulic Research, Zhengzhou, 45003, China
Pengcheng Sun
Key Laboratory of Soil and Water Conservation on the Loess Plateau, Yellow River Institute of Hydraulic Research, Yellow River Conservancy Commission, Zhengzhou, 450003, China
Feng Feng
Yellow River Conservancy Technical Institute, Kaifeng, 475004, China
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Total article views: 2,583 (including HTML, PDF, and XML)
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Total article views: 3,427 (including HTML, PDF, and XML)
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Total article views: 2,583 (including HTML, PDF, and XML)
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Total article views: 844 (including HTML, PDF, and XML)
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Variable infiltration capacity simulation considering dynamic vegetation types and structural parameters is able to better capture the effect of temporally explicit vegetation change and climate variation in hydrological regimes. Vegetation greening including interannual LAI and intra-annual LAI temporal pattern change induced by large-scale ecological restoration and non-vegetation underlying surface change played dominant roles in the natural streamflow reduction of the Yellow River basin.
Variable infiltration capacity simulation considering dynamic vegetation types and structural...
