globalchange  > 气候变化与战略
DOI: 10.5194/hess-23-549-2019
论文题名:
Emergent stationarity in Yellow River sediment transport and the underlying shift of dominance: From streamflow to vegetation
作者: Ye S.; Ran Q.; Fu X.; Hu C.; Wang G.; Parker G.; Chen X.; Zhang S.
刊名: Hydrology and Earth System Sciences
ISSN: 1027-5606
出版年: 2019
卷: 23, 期:1
起始页码: 549
结束页码: 556
语种: 英语
Scopus关键词: Biogeochemistry ; Erosion ; Gages ; Sediment transport ; Stream flow ; Vegetation ; Biogeochemical cycle ; Controlling factors ; Human intervention ; Normalized difference vegetation index ; Sediment concentration ; Terrestrial landscape ; Vegetation resistance ; Yellow River basin ; Sedimentation ; gauge ; heterogeneity ; NDVI ; river discharge ; sediment transport ; soil erosion ; streamflow ; vegetation ; water erosion ; China ; Yellow River Basin
英文摘要: Soil erosion and sediment transport play important roles in terrestrial landscape evolution and biogeochemical cycles of nutrients and contaminants. Although discharge is considered to be a controlling factor in sediment transport, its correlation with sediment concentration varies across the Yellow River basin (YRB) and is not fully understood. This paper provides analysis from gauges across the YRB covering a range of climates, topographic characteristics, and degrees of human intervention. Our results show that discharge control on sediment transport is dampened at gauges with large mean annual discharge, where sediment concentration becomes more and more stable. This emergent stationarity can be attributed to vegetation resistance. Our analysis shows that sediment concentration follows a bell shape with vegetation index (normalized difference vegetation index, NDVI) at an annual scale despite heterogeneity in climate and landscape. We obtain the counterintuitive result that, as mean annual discharge increases, the dominant control on sediment transport shifts from streamflow erosion to vegetation retardation in the YRB. © 2019 Copernicus GmbH. All rights reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/163065
Appears in Collections:气候变化与战略

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作者单位: Ye, S., Institute of Hydrology and Water Resources, Department of Hydraulic Engineering, Zhejiang University, Hangzhou, 310058, China; Ran, Q., Institute of Hydrology and Water Resources, Department of Hydraulic Engineering, Zhejiang University, Hangzhou, 310058, China; Fu, X., State Key Laboratory of Hydro-science and Engineering, Tsinghua University, Beijing, 100084, China; Hu, C., State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Institute of Water Resources and Hydropower Research, Beijing, 100048, China; Wang, G., State Key Laboratory of Hydro-science and Engineering, Tsinghua University, Beijing, 100084, China; Parker, G., Department of Civil and Environmental Engineering and Department of Geology, University of Illinois at Urbana-Champaign, Urbana, IL 61801, United States; Chen, X., Institute of Hydrology and Water Resources, Department of Hydraulic Engineering, Zhejiang University, Hangzhou, 310058, China; Zhang, S., Institute of Hydrology and Water Resources, Department of Hydraulic Engineering, Zhejiang University, Hangzhou, 310058, China

Recommended Citation:
Ye S.,Ran Q.,Fu X.,et al. Emergent stationarity in Yellow River sediment transport and the underlying shift of dominance: From streamflow to vegetation[J]. Hydrology and Earth System Sciences,2019-01-01,23(1)
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