Natural short-lived halogens exert an indirect cooling effect on climate

被引:45
作者
Saiz-Lopez, Alfonso [1 ]
Fernandez, Rafael P. P. [1 ,2 ]
Li, Qinyi [1 ,12 ]
Cuevas, Carlos A. A. [1 ]
Fu, Xiao [3 ]
Kinnison, Douglas E. E. [4 ]
Tilmes, Simone [4 ]
Mahajan, Anoop S. S. [5 ]
Gomez Martin, Juan Carlos [6 ]
Iglesias-Suarez, Fernando [7 ]
Hossaini, Ryan [8 ]
Plane, John M. C. [9 ]
Myhre, Gunnar [10 ]
Lamarque, Jean-Francois [11 ]
机构
[1] CSIC, Inst Phys Chem Rocasolano, Dept Atmospher Chem & Climate, Madrid, Spain
[2] Natl Res Council CONICET, FCEN UNCuyo, Inst Interdisciplinary Sci ICB, Mendoza, Argentina
[3] Tsinghua Univ, Tsinghua Shenzhen Int Grad Sch, Inst Environm & Ecol, Shenzhen, Peoples R China
[4] Natl Ctr Atmospher Res, Atmospher Chem Observat & Modeling Lab, Boulder, CO USA
[5] Minist Earth Sci, Indian Inst Trop Meteorol, Ctr Climate Change Res, Pune, India
[6] CSIC, Inst Astrofis Andalucia, Granada, Spain
[7] Inst Phys Atmosphare, Deutsch Zent Luft & Raumfahrt DLR, Oberpfaffenhofen, Germany
[8] Univ Lancaster, Lancaster Environm Ctr, Lancaster, England
[9] Univ Leeds, Sch Chem, Leeds, England
[10] CICERO Ctr Int Climate Res, Oslo, Norway
[11] Natl Ctr Atmospher Res, Climate & Global Dynam Lab, Boulder, CO USA
[12] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Hong Kong, Peoples R China
基金
欧洲研究理事会; 美国国家科学基金会;
关键词
IODINE CHEMISTRY; ANTHROPOGENIC EMISSIONS; ATMOSPHERIC CHEMISTRY; PARTICULATE MATTER; BROMINE CHEMISTRY; GLOBAL EMISSIONS; REACTIVE HALOGEN; AIR-POLLUTANTS; OZONE; MODEL;
D O I
10.1038/s41586-023-06119-z
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Observational evidence shows the ubiquitous presence of ocean-emitted short-lived halogens in the global atmosphere(1-3). Natural emissions of these chemical compounds have been anthropogenically amplified since pre-industrial times(4-6), while, in addition, anthropogenic short-lived halocarbons are currently being emitted to the atmosphere(7,8). Despite their widespread distribution in the atmosphere, the combined impact of these species on Earth's radiative balance remains unknown. Here we show that short-lived halogens exert a substantial indirect cooling effect at present (-0.13 +/- 0.03 watts per square metre) that arises from halogen-mediated radiative perturbations of ozone (-0.24 +/- 0.02 watts per square metre), compensated by those from methane (+0.09 +/- 0.01 watts per square metre), aerosols (+0.03 +/- 0.01 watts per square metre) and stratospheric water vapour (+0.011 +/- 0.001 watts per square metre). Importantly, this substantial cooling effect has increased since 1750 by -0.05 +/- 0.03 watts per square metre (61 per cent), driven by the anthropogenic amplification of natural halogen emissions, and is projected to change further (18-31 per cent by 2100) depending on climate warming projections and socioeconomic development. We conclude that the indirect radiative effect due to short-lived halogens should now be incorporated into climate models to provide a more realistic natural baseline of Earth's climate system.
引用
收藏
页码:967 / 973
页数:7
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