干旱区生态环境知识资源中心(Arid): Temporal Scaling of Streamflow Elasticity to Precipitation: A Global Analysis

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DOI	10.1029/2021WR030601
	Temporal Scaling of Streamflow Elasticity to Precipitation: A Global Analysis
	Zhang, Yongqiang; Viglione, Alberto; Bloeschl, Gunter
通讯作者	Zhang, YQ (corresponding author)，Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing, Peoples R China.
来源期刊	WATER RESOURCES RESEARCH
ISSN	0043-1397
EISSN	1944-7973
出版年	2022
卷号	58 期号:1
英文摘要	Streamflow elasticity to precipitation, defined as the percent change of streamflow resulting from a 1% change in precipitation, is sometimes used as an alternative to rainfall-runoff models in climate impact analyses. Elasticity is usually estimated from long streamflow and precipitation series aggregated at annual time steps while the climate impact analyses are usually geared toward changes at decadal scales. The purpose of this paper is therefore to understand how the elasticity depends on the aggregation time scale and the process controls of such a dependence. We analyze streamflow records of 7,053 catchments around the world over the period 1950-2016, and select 5,327 with reliable elasticity estimates for aggregation time ranging from 13 to 60 months. We find a significant scaling of streamflow elasticity to precipitation with aggregation time in 66% of the catchments which is much larger than expected by chance. Positive scaling occurs much more frequently than negative scaling. More arid/less rainy catchments, less forested catchments and catchments with a large base flow contribution to streamflow are more frequently characterized by a positive scaling. A random forest classification model identifies aridity index, latitude, mean annual precipitation, the potential evapotranspiration seasonality, the base flow index and the precipitation seasonality as relevant explanatory variables of the scaling. We interpret the sign of the scaling by non-linear runoff generation in arid regions, by the effect of climate modes and snow processes, and by the regulation capacity of vegetation to transpire more water if the past years were wet. It is suggested to use decadal elasticities instead of annual elasticities in climate impact analyses in order to account for their scaling behavior.
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000751310200027
WOS关键词	CLIMATE ELASTICITY ; CATCHMENT SCALE ; STORAGE ; SENSITIVITY ; DROUGHT ; COEVOLUTION ; VARIABILITY ; TRENDS ; FLOW
WOS类目	Environmental Sciences ; Limnology ; Water Resources
WOS研究方向	Environmental Sciences & Ecology ; Marine & Freshwater Biology ; Water Resources
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/376704
作者单位	[Zhang, Yongqiang] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing, Peoples R China; [Viglione, Alberto] Politecn Torino, Dept Environm Land & Infrastruct Engn, Turin, Italy; [Bloeschl, Gunter] Tech Univ Wien, Inst Hydraul & Water Resources Engn, Vienna, Austria
推荐引用方式 GB/T 7714	Zhang, Yongqiang,Viglione, Alberto,Bloeschl, Gunter. Temporal Scaling of Streamflow Elasticity to Precipitation: A Global Analysis[J],2022,58(1).
APA	Zhang, Yongqiang,Viglione, Alberto,&Bloeschl, Gunter.(2022).Temporal Scaling of Streamflow Elasticity to Precipitation: A Global Analysis.WATER RESOURCES RESEARCH,58(1).
MLA	Zhang, Yongqiang,et al."Temporal Scaling of Streamflow Elasticity to Precipitation: A Global Analysis".WATER RESOURCES RESEARCH 58.1(2022).