Evaluating the effects of single and integrated extreme climate events on hydrology in the Liao River Basin, China using a modified SWAT-BSR model

被引:4
|
作者
Zhang, Yingqi [1 ,2 ,3 ]
Ge, Jianing [1 ,2 ,3 ]
Qi, Junyu [4 ]
Liu, Haipeng [1 ,2 ]
Zhang, Xueliang [1 ,3 ]
Marek, Gary W. [5 ]
Yuan, Chengcheng [1 ,3 ]
Ding, Beibei [1 ,3 ]
Feng, Puyu [1 ,2 ]
Liu, De Li [6 ,7 ]
Srinivasan, Raghavan [8 ]
Chen, Yong [1 ,2 ,3 ]
机构
[1] China Agr Univ, Coll Land Sci & Technol, Beijing 100193, Peoples R China
[2] Minist Agr & Rural Affairs, Key Lab Arable Land Conservat North China, Beijing 100193, Peoples R China
[3] China Agr Univ, Res Ctr Land Use & Management, Beijing 100193, Peoples R China
[4] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20740 USA
[5] USDA ARS, Conservat & Prod Res Lab, Bushland, TX 79012 USA
[6] Wagga Wagga Agr Inst, NSW Dept Primary Ind, Wagga Wagga, NSW 2650, Australia
[7] Univ New South Wales, Climate Change Res Ctr, Sydney 2052, Australia
[8] Texas A&M Univ, Dept Ecosyst Sci & Management, College Stn, TX 77843 USA
基金
美国食品与农业研究所;
关键词
Extreme climate events; Future climate change; CMIP6; SWAT-BSR; Hydrological cycle; SPATIOTEMPORAL VARIABILITY; TEMPERATURE; EVAPOTRANSPIRATION; PRECIPITATION; IMPACTS;
D O I
10.1016/j.jhydrol.2023.129772
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Extreme climate events may have a substantial impact on water conservation in the black soil region of China. This study integrated a dynamic CO2 input method and an alternative freeze-thaw cycle function into Soil and Water Assessment Tool (SWAT) to create a SWAT-Black Soil Region (SWAT-BSR) model. The SWAT-BSR model was used to simulate extreme climate events in the Liao River Basin (LRB; 220,000 km2) and an R script was developed to extract days in which extreme climate events occurred along with corresponding hydrological variables. Extreme climate events included extreme heat, cold, precipitation, and drought events across seven zones in the LRB. Subsequently, we explored the changes in single and integrated extreme climate events during the historical period (1971-2000) and future periods (2041-2070 and 2071-2100) under the SSP2-4.5 and SSP58.5 scenarios. The results indicated that almost each hydrological variable was reduced under extreme cold and drought events compared to the normal conditions in the historical period. Canopy interception and percolation were decreased under extreme heat in the future periods while extreme cold was opposite with a pronounced negative impact on reference evapotranspiration and soil evaporation. In contrast, each hydrological variable under extreme precipitation increased relative to the normal conditions while hydrological variables were largely negatively affected under extreme drought. In addition, the integrated extreme climate index increased over time, with more pronounced changes under the SSP5-8.5 scenario than those of SSP2-4.5 scenario. Hydrological variables were most at risk in the dryland zones as compared to partially irrigated and irrigated zones. These findings indicated that more attention should be given to the impacts of extreme climate events on water losses from both historical and future perspectives. It is also necessary to develop mitigation strategies for water conservation in the LRB based on the extreme climate events projected to occur in different zones and periods in the future.
引用
收藏
页数:16
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