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量化美国中西部灌溉对玉米产量的冷却效益。

Quantifying irrigation cooling benefits to maize yield in the US Midwest.

机构信息

State Key Laboratory of Earth Surface Processes and Resources Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China.

Department of Natural Resources and Environmental Sciences, University of Illinois at Urbana-Champaign, Urbana, IL, USA.

出版信息

Glob Chang Biol. 2020 May;26(5):3065-3078. doi: 10.1111/gcb.15002. Epub 2020 Mar 13.

Abstract

Irrigation is an important adaptation strategy to improve crop resilience to global climate change. Irrigation plays an essential role in sustaining crop production in water-limited regions, as irrigation water not only benefits crops through fulfilling crops' water demand but also creates an evaporative cooling that mitigates crop heat stress. Here we use satellite remote sensing and maize yield data in the state of Nebraska, USA, combined with statistical models, to quantify the contribution of cooling and water supply to the yield benefits due to irrigation. Results show that irrigation leads to a considerable cooling on daytime land surface temperature (-1.63°C in July), an increase in enhanced vegetation index (+0.10 in July), and 81% higher maize yields compared to rainfed maize. These irrigation effects vary along the spatial and temporal gradients of precipitation and temperature, with a greater effect in dry and hot conditions, and decline toward wet and cool conditions. We find that 16% of irrigation yield increase is due to irrigation cooling, while the rest (84%) is due to water supply and other factors. The irrigation cooling effect is also observed on air temperature (-0.38 to -0.53°C) from paired flux sites in Nebraska. This study highlights the non-negligible contribution of irrigation cooling to the yield benefits of irrigation, and such an effect may become more important in the future with continued warming and more frequent droughts.

摘要

灌溉是提高作物对全球气候变化适应能力的重要策略。在水资源有限的地区,灌溉在维持作物生产方面起着至关重要的作用,因为灌溉水不仅通过满足作物的水分需求使作物受益,还通过蒸发冷却减轻作物热应激。在这里,我们使用卫星遥感和美国内布拉斯加州的玉米产量数据,结合统计模型,定量评估了冷却和供水对灌溉带来的产量增益的贡献。结果表明,与雨养玉米相比,灌溉导致白天陆地表面温度显著降低(7 月降低 1.63°C),增强植被指数增加(7 月增加 0.10),玉米产量增加 81%。这些灌溉效应随降水和温度的时空梯度而变化,在干燥和炎热的条件下效应更大,而在湿润和凉爽的条件下则逐渐减弱。我们发现,灌溉增产的 16%归因于灌溉冷却,其余 84%归因于供水和其他因素。在内布拉斯加州的通量对站点也观察到了灌溉对空气温度(-0.38 至-0.53°C)的冷却效应。本研究强调了灌溉冷却对灌溉产量增益的不可忽视的贡献,随着持续变暖以及干旱更加频繁,这种效应在未来可能变得更加重要。

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