Articles | Volume 26, issue 20
Hydrol. Earth Syst. Sci., 26, 5291–5314, 2022
https://doi.org/10.5194/hess-26-5291-2022
Hydrol. Earth Syst. Sci., 26, 5291–5314, 2022
https://doi.org/10.5194/hess-26-5291-2022
Research article
26 Oct 2022
Research article | 26 Oct 2022

Attributing trend in naturalized streamflow to temporally explicit vegetation change and climate variation in the Yellow River basin of China

Zhihui Wang et al.

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Cited articles

Aerospace Information Research Institute and Chinese Academy of Sciences: Global Land-cover Product with Fine Classification System, Aerospace Information Research Institute and Chinese Academy of Sciences, http://www.geodata.cn/, last access: 4 November 2021. 
Bai, M., Mo, X., Liu, S., and Hu, S.: Contributions of climate change and vegetation greening to evapotranspiration trend in a typical hilly-gully basin on the Loess Plateau: China, Sci. Total Environ., 657, 325–339, https://doi.org/10.1016/j.scitotenv.2018.11.360, 2018. 
Bai, J., Yang, S., Zhang, Y., Liu, X., and Guan, Y.: Assessing the Impact of Terraces and Vegetation on Runoff and Sediment Routing Using the Time-Area Method in the Chinese Loess Plateau, Water, 11, 803, https://doi.org/10.3390/w11040803, 2019. 
Bao, Z., Zhang, J., Wang, G., Chen, Q., Guan, T., Yan, X., Liu, G., Liu, J., and Wang, J.: The impact of climate variability and land use/cover change on the water balance in the Middle Yellow River Basin, China, J. Hydrol., 577, 123942, https://doi.org/10.1016/j.jhydrol.2019.123942, 2019. 
Beijing Normal Universtiy: Global Land Surface Satellite (GLASS) LAI Product (v5.0), Beijing Normal Universtiy, http://glass-product.bnu.edu.cn/, last access: 7 January 2020. 
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Short summary
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.