Improving hydrological modeling to close the gap between elevated CO2 concentration and crop response: Implications for water resources

被引:3
作者
Wen, Na [1 ]
Han, Yiwen [1 ]
Qi, Junyu [2 ]
Marek, Gary W. [3 ]
Sun, Danfeng [1 ]
Feng, Puyu [1 ]
Srinivasan, Raghavan [4 ]
Li Liu, De [5 ,6 ]
Chen, Yong [1 ]
机构
[1] China Agr Univ, Coll Land Sci & Technol, State Key Lab Efficient Utilizat Agr Water Resourc, Beijing 100083, Peoples R China
[2] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20740 USA
[3] USDA ARS, Conservat & Prod Res Lab, Bushland, TX 79012 USA
[4] Texas A&M Univ, Dept Ecosyst Sci & Management, College Stn, TX 77843 USA
[5] Wagga Wagga Agr Inst, NSW Dept Primary Ind, Wagga Wagga, NSW 2650, Australia
[6] Univ New South Wales, Climate Change Res Ctr, Sydney, NSW 2052, Australia
基金
美国食品与农业研究所;
关键词
Climate change; Elevated CO 2 concentrations; Evapotranspiration; Leaf area index; Stomatal conductance; SWAT-CO; 2; model; CLIMATE-CHANGE; EPIC MODEL; PLANT-RESPONSES; QUALITY MODELS; IMPACTS; EVAPOTRANSPIRATION; PERFORMANCE; PLAINS; MAIZE; YIELD;
D O I
10.1016/j.watres.2024.122279
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Rising atmospheric carbon dioxide concentrations ([CO2]) affect crop growth and the associated hydrological cycle through physiological forcing, which is mainly regulated by reducing stomatal conductance (gs) and increasing leaf area index (LAI). However, reduced gs and increased LAI can affect crop water consumption, and the overall effects need to be quantified under elevated [CO2]. Here we develop a SWAT-gs-LAI model by incorporating a nonlinear gs-CO2 equation and a missing LAI-CO2 relationship to investigate the responses of water consumption of grain maize, maize yield, and losses of water and soil to elevated [CO2] in the Upper Mississippi River Basin (UMRB; 492,000 km2). Results exhibited enhanced maize yield with decreased water consumption for increases in [CO2] from 495 ppm to 825 ppm during the historical period (1985-2014). Elevated [CO2] promoted surface runoff but suppressed sediment loss as the predominant impact of LAI-CO2 leading to enhanced surface cover. A comprehensive analysis of future climate change showed increased maize water consumption in comparison to the historical period, driven by the more pronounced effects of overall climate change rather than solely elevated [CO2]. Generally, future climate change promoted maize yield in most regions of the UMRB for three Shared Socioeconomic Pathway (SSP) scenarios. Surface runoff was shown to increase generally in the future with sediment loss increasing by an average of 0.39, 0.42, and 0.66 ton ha-1 for SSP1-2.6, SSP2-4.5, and SSP5-8.5, respectively. This was due to negative climatic change effects largely surpassing the positive effect of elevated [CO2], particularly in zones near the middle and lower stream. Our results underscore the crucial role of employing a physically-based model to represent crop physiological processes under elevated [CO2] conditions, improving the reliability of predictions related to crop growth and the hydrological cycle.
引用
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页数:14
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