中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Majority of global river flow sustained by groundwater

文献类型:期刊论文

作者Xie, Jiaxin2,3,5; Liu, Xiaomang3; Jasechko, Scott1; Berghuijs, Wouter R.4; Wang, Kaiwen3; Liu, Changming3; Reichstein, Markus5,6; Jung, Martin5; Koirala, Sujan5
刊名NATURE GEOSCIENCE
出版日期2024-07-19
卷号N/A
DOI10.1038/s41561-024-01483-5
产权排序1
文献子类Article ; Early Access
英文摘要Groundwater-sustained baseflow is a vital source of river flow, especially during dry seasons. The proportion of river flow sustained by baseflow-the baseflow index-is essential for assessing fluvial nutrient cycling and contaminant transport. However, the global baseflow index remains highly uncertain, with current Earth system model simulations ranging from 12% to 94%. Here we estimate the global baseflow index to be 59% +/- 7% based on an emergent constraint approach, which integrates 50 Earth system models with baseflow indices derived from streamflow observations in 15,567 basins. Our observational constraint indicates that at least 21% +/- 3% of precipitation recharges groundwater, which is approximately double the figure reported in the Sixth Assessment Report of the United Nations Intergovernmental Panel on Climate Change. Thus, our research suggests a more active role of groundwater in the global water cycle than most Earth system models currently simulate. We present evidence that the considerable disagreement in simulated baseflow stems from unrealistic and varied model representations of infiltration, aquifer structure and groundwater dynamics. These processes should be prioritized so that models can capture active groundwater-river connections. Groundwater supplies about 59% of global river flow, suggesting a larger contribution of groundwater to the global water cycle than currently appreciated, according to an analysis integrating estimates from models and observations.
WOS关键词COMMUNITY LAND MODEL ; BASE-FLOW ; EMERGENT CONSTRAINTS ; AUTOMATED TECHNIQUES ; WATER-RESOURCES ; TECHNICAL NOTE ; STREAMFLOW ; SENSITIVITY ; SEPARATION ; INDEX
WOS研究方向Geology
WOS记录号WOS:001272944300001
源URL[http://ir.igsnrr.ac.cn/handle/311030/206146]  
专题陆地水循环及地表过程院重点实验室_外文论文
通讯作者Liu, Xiaomang
作者单位1.Univ Calif Santa Barbara, Bren Sch Environm Sci & Management, Santa Barbara, CA USA
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing, Peoples R China
4.Free Univ Amsterdam, Dept Earth Sci, Amsterdam, Netherlands
5.Max Planck Inst Biogeochem, Dept Biogeochem Integrat, Jena, Germany
6.ELLIS Unit Jena, Jena, Germany
推荐引用方式
GB/T 7714
Xie, Jiaxin,Liu, Xiaomang,Jasechko, Scott,et al. Majority of global river flow sustained by groundwater[J]. NATURE GEOSCIENCE,2024,N/A.
APA Xie, Jiaxin.,Liu, Xiaomang.,Jasechko, Scott.,Berghuijs, Wouter R..,Wang, Kaiwen.,...&Koirala, Sujan.(2024).Majority of global river flow sustained by groundwater.NATURE GEOSCIENCE,N/A.
MLA Xie, Jiaxin,et al."Majority of global river flow sustained by groundwater".NATURE GEOSCIENCE N/A(2024).

入库方式: OAI收割

来源:地理科学与资源研究所

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