エアロゾル削減、温室効果ガスと同様にモンスーン地域の水資源に重要な影響(Aerosol Reduction Equally Critical as GHGs in Shaping Water Availability in Global Monsoon Regions, Study Finds)

2025-07-18 中国科学院(CAS)

中国科学院大気物理研究所の研究によると、将来のモンスーン地域における水資源(降水-蒸発:P–E)の変化には、温室効果ガス(GHG)だけでなくエアロゾル削減も同等に重要な役割を果たす。Science Bulletinに掲載された本研究は、1951~2100年のP–E変化をSSP2-4.5シナリオで分析。GHGの増加はアジア・アフリカでP–Eを増加、アメリカ地域では減少させる。一方、エアロゾルの減少は乾燥傾向を逆転させ湿潤化を促進し、アジア・アフリカではGHGと同程度の影響を与える。大気循環や雲との相互作用が地域差の背景にあり、研究者は水資源管理においてGHG対策と大気浄化の両立が必要と強調している。

<関連情報>

エアロゾルの緩和は、地球モンスーン地域における将来の水利用可能性に重要である Aerosol mitigation matters to future water availability in the global monsoon region

Jie Jiang, Tianjun Zhou, Wenxia Zhang
Science Bulletin  Available online: 21 May 2025
DOI:https://doi.org/10.1016/j.scib.2025.05.023

Graphical abstract

エアロゾル削減、温室効果ガスと同様にモンスーン地域の水資源に重要な影響(Aerosol Reduction Equally Critical as GHGs in Shaping Water Availability in Global Monsoon Regions, Study Finds)

Abstract

Water availability, as measured by precipitation minus evaporation (P–E), is projected to increase in the 21st century across the global monsoon region. However, while the impacts of increased greenhouse gas (GHG) concentrations are highlighted in existing studies, the contribution of reduced anthropogenic aerosol (AA) emissions is likely to be overlooked. Here, utilizing single-forcing projections under the SSP2-4.5 scenario, we elucidate the fingerprints of GHG and AA forcings on future P–E evolution. We reveal that future P–E changes are primarily driven by changes during the wet season, with contrasting trends between the Asian-African and American monsoon domains. The escalation of GHG concentrations is projected to increase P–E over Asian–African monsoon domains while decreasing it over the American monsoon domains. Conversely, aerosol reductions will drive a transition from current widespread drying to future wetting, with contributions comparable to GHG forcing over the Asian-African monsoon domains. While GHG increases and AA reductions can elevate atmospheric moistening through radiative warming, the disparate P–E responses arise from dynamic processes that favor drying trends in the American monsoon domains under GHG forcing. In contrast, strengthened monsoon circulations contribute to a wetting trend in the Asian-African monsoon domains under AA reductions, attributable to greater interhemispheric thermal contrast. Our findings highlight the importance of considering aerosol mitigation in climate risk assessments for densely populated monsoon regions.

1702地球物理及び地球化学
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