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Frontiers of Agricultural Science and Engineering

ISSN 2095-7505

ISSN 2095-977X(Online)

CN 10-1204/S

Postal Subscription Code 80-906

Front. Agr. Sci. Eng.    2024, Vol. 11 Issue (4) : 515-526    https://doi.org/10.15302/J-FASE-2024574
Impact of climate extremes on agricultural water scarcity and the spatial scale effect
Jiongjiong LIU1,2,3, Yilin ZHAO1,2,3, Wenfeng LIU1,2,3()
. State Key Laboratory of Efficient Utilization of Agricultural Water Resources, Beijing 100083, China
. National Field Scientific Observation and Research Station on Efficient Water Use of Oasis Agriculture in Wuwei of Gansu Province, Wuwei 733000, China
. Center for Agricultural Water Research in China, College of Water Resources and Civil Engineering, China Agricultural University, Beijing 100083, China
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Abstract

Amid the escalating frequency of climate extremes, it is crucial to determine their impact on agricultural water scarcity to preserve agricultural development. Current research does not often examine how different spatial scales and compound climate extremes influence agricultural water scarcity. Using an agricultural water scarcity index (AWSI), this study examined the effects of precipitation and temperature extremes on AWSI across secondary and tertiary river basins in China from 1971 to 2010. The results indicated a marked increase in AWSI during dry years and elevated temperatures. The analysis underscores that precipitation had a greater impact on AWSI than temperature variation. In secondary basins, AWSI was about 26% higher than the long-term average during dry years, increasing to nearly 49% in exceptionally dry conditions. By comparison, in tertiary basins, the increases were 28% and 55%, respectively. In hot years, AWSI rose by about 6.8% (7.3% for tertiary basins) above the average, surging to about 19.1% (15.5% for tertiary basins) during extremely hot periods. These results show that AWSI assessment at the tertiary basin level better captured the influence of climate extremes on AWSI than assessments at the secondary basin level, which highlights the critical importance of a finer spatial scale for a more precise assessment and forecast of water scarcity within basin scales. Also, this study has highlighted the paramount urgency of implementing strategies to tackle water scarcity issues under compound extreme dry and hot conditions. Overall, this study offers an in-depth evaluation of the influence of both precipitation and temperature variation, and research scale on water scarcity, which will help formulate better water resource management strategies.

Keywords Agricultural water scarcity      compound climate extremes      spatial scale effect      river basin     
Corresponding Author(s): Wenfeng LIU   
Online First Date: 20 September 2024    Issue Date: 12 November 2024
 Cite this article:   
Jiongjiong LIU,Yilin ZHAO,Wenfeng LIU. Impact of climate extremes on agricultural water scarcity and the spatial scale effect[J]. Front. Agr. Sci. Eng. , 2024, 11(4): 515-526.
 URL:  
https://academic.hep.com.cn/fase/EN/10.15302/J-FASE-2024574
https://academic.hep.com.cn/fase/EN/Y2024/V11/I4/515
Fig.1  Distribution of annual average precipitation and temperature for secondary (a, c) and tertiary (b, d) river basins (审图号: GS 京(2024)1698号).
Fig.2  Average agricultural water scarcity index (AWSI) in China from 1971 to 2010 aggregated to secondary (a) and tertiary (b) river basin levels (审图号: GS 京(2024)1698号).
Fig.3  Relative changes in agricultural water scarcity index (AWSI) resulting from precipitation and temperature anomalies across secondary (a) and tertiary (b) river basins. The datasets comprise 2320 and 8480 basin-year samples for secondary and tertiary river basins, respectively.
Fig.4  Variations in the agricultural water scarcity index (AWSI) in response to precipitation and temperature anomalies. Each subplot illustrates the overall relative change (%) in AWSI, adjusted for basin areas, using data from basin-year samples. Error bars in the graphs represent a 95% confidence intervals, calculated from 1000 bootstrap estimates. Years with precipitation anomalies lower than ?1.0 standard deviation (σ) are classified as dry years whereas those with anomalies higher than 1.0σ are considered wet years for secondary (a) and tertiary (b) river basins. Similarly, temperature anomalies below ?1.0σ categorize years as cold and those above 1.0σ as hot for secondary (c) and tertiary (d) river basins.
Fig.5  Basin-year sample ratios (%) with different precipitation and temperature anomalies for secondary (a, c) and tertiary (b, d) river basins.
Fig.6  Relative changes (RC) in agricultural water scarcity index (AWSI) from multiyear averages under dry and hot conditions for secondary and tertiary basins (审图号: GS 京(2024)1698号). Dry conditions for secondary (a) and tertiary (b) basins, and hot conditions for secondary (c) and tertiary (d) basins.
Fig.7  Relative changes (RC) in agricultural water scarcity index (AWSI) from multiyear averages under compound dry and hot conditions for secondary (a) and tertiary (b) river basins (审图号: GS 京(2024)1698号). White color indicates no compound dry and hot conditions.
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