Compounding future escalation of emissions- and irrigation-induced increases in humid-heat stress.

IF 15.7 1区 综合性期刊 Q1 MULTIDISCIPLINARY SCIENCES
Yi Yao,Yusuke Satoh,Nicole van Maanen,Sabin Taranu,Jessica Keune,Steven J De Hertog,Seppe Lampe,David M Lawrence,William J Sacks,Yoshihide Wada,Agnès Ducharne,Benjamin I Cook,Sonia I Seneviratne,Laibao Liu,Jonathan R Buzan,Jonas Jägermeyr,Wim Thiery
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Abstract

Irrigation has been investigated as an important historical climate forcing, but there is no study exploring its future climatic impacts considering possible changes in both extent and efficiency. Here, we address these issues via developing irrigation efficiency scenarios in line with the Shared Socioeconomic Pathways (SSPs), implementing these in the Community Earth System Model, and applying them to generate projections over the period 2015-2074. We project that annual irrigation water withdrawal decreases under SSP1-2.6 (from ~2100 to ~1700 km3 yr-1) but increases under SSP3-7.0 (to ~2400 km3 yr-1), with some new irrigation hot spots emerging, especially in Africa. Irrigation is projected to reduce the occurrence of dry-heat stress under both scenarios, but cannot reverse the warming trend due to greenhouse gas emission (e.g., increasing from ~90 to around 600 and 1200 hours yr-1 in intensely irrigated areas, under two scenarios). Moreover, moist-heat extreme event frequency increases more substantially (by ≥1600 hours yr-1 under SSP3-7.0 in tropical regions), and irrigation further amplifies the hours of exposure (for example, by ≥100 hours yr-1 in South Asia), thereby raising the risk of moist-heat-related illnesses and mortality for exposed communities. Our results underscore the importance of reducing greenhouse gas emissions, limiting irrigation expansion and improving irrigation efficiency to preserve water resources and decelerate escalating exposure to dry- and moist-heat stress.
使排放和灌溉引起的湿热压力增加的未来升级更加复杂。
灌溉作为一种重要的历史气候强迫已被研究,但考虑其在程度和效率上可能发生的变化,尚未有研究探讨其对未来气候的影响。在这里,我们通过开发符合共享社会经济路径(ssp)的灌溉效率情景来解决这些问题,在社区地球系统模型中实施这些情景,并应用它们生成2015-2074年期间的预测。我们预测SSP1-2.6下的年灌溉取水量减少(从~2100 ~1700 km3 -1),而SSP3-7.0下的年灌溉取水量增加(到~2400 km3 -1),并出现一些新的灌溉热点,特别是在非洲。在两种情景下,灌溉水预估可减少干热胁迫的发生,但不能逆转温室气体排放造成的变暖趋势(例如,在两种情景下,强烈灌溉区从每年约90小时增加到每年约600和1200小时)。此外,湿热极端事件频率的增加更为显著(热带地区在SSP3-7.0下每年增加≥1600小时),灌溉进一步增加了暴露时间(例如,在南亚每年增加≥100小时),从而增加了暴露社区患湿热相关疾病和死亡率的风险。我们的研究结果强调了减少温室气体排放、限制灌溉扩张和提高灌溉效率对保护水资源和减缓干旱和湿热胁迫的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Nature Communications
Nature Communications Biological Science Disciplines-
CiteScore
24.90
自引率
2.40%
发文量
6928
审稿时长
3.7 months
期刊介绍: Nature Communications, an open-access journal, publishes high-quality research spanning all areas of the natural sciences. Papers featured in the journal showcase significant advances relevant to specialists in each respective field. With a 2-year impact factor of 16.6 (2022) and a median time of 8 days from submission to the first editorial decision, Nature Communications is committed to rapid dissemination of research findings. As a multidisciplinary journal, it welcomes contributions from biological, health, physical, chemical, Earth, social, mathematical, applied, and engineering sciences, aiming to highlight important breakthroughs within each domain.
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