China’s SO <sub>2</sub> emission reductions enhance atmospheric ozone–driven sulfate aerosol production in East Asia

Y Yu-Chi Lin (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) Y Yan Zhao Y Yan-Lin Zhang (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) Y Yihang Hong (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) S Shohei Hattori (International Center for Isotope Effects Research, Nanjing University) S Syuichi Itahashi (Research Institute for Applied Mechanics, Kyushu University) M Mei-Yi Fan (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) F Feng Xie Z Zhu-Yu Zhao (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) M Mingyuan Yu (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) F Fang Cao (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) R Rongshuang Xu (Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology) J Jianghanyang Li (Institute of Arctic and Alpine Research, University of Colorado) K Kimitaka Kawamura (Chubu Institute for Advanced Study, Chubu University) M Mark H. Thiemens (Department of Chemistry and Biochemistry, University of California)

Abstract

Reduction of China’s SO 2 emissions has been found to nonlinearly decrease the atmospheric sulfate (SO 4 2− ) aerosol concentrations in East Asia. Compared to Europe and North America, the lower effectiveness of SO 4 2− reduction in East Asia suggested much effects of “acidity-sensitive” feedback mechanisms in this high anthropogenic emission region, which have not been yet examined. In this work, we investigated these feedback mechanisms in East Asia through long-term measurements of the mass-independent oxygen-17 anomaly (Δ 17 O) in sulfate aerosols, machine learning and Community Multiscale Air Quality (CMAQ) model. As China’s emissions reduced, the atmospheric acidity decreased, enhancing the ozone-driven oxidation of S(IV) and production efficiency of sulfate formation. This explained the weaker declining SO 4 2− concentrations than SO 2 emissions. By the evidence from observed Δ 17 O in non-sea-salt sulfate (Δ 17 O-nss-SO 4 2− ) and CMAQ simulations, the highly enhanced contributions of S(IV)+O 3 to sulfate driven by reduced SO 2 emissions explained the low effectiveness of SO 4 2− reduction in East Asia. Additionally, the decreases of acidity by substantial NH 3 emissions are projected to continue until 2050, limiting SO 4 2− reduction effectiveness. Thus, we highlighted that global control of both SO 2 and NH 3 emissions are needed to efficiently mitigate the sulfate-related climate and pollution, especially in high NH 3 emission region, such as East Asia.

Article Details

Volume / Issue Vol. 122, Issue 24
Published June 17, 2025
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (15)

Y

Yu-Chi Lin

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

Y

Yan Zhao

Y

Yan-Lin Zhang

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

Y

Yihang Hong

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

S

Shohei Hattori

International Center for Isotope Effects Research, Nanjing University

S

Syuichi Itahashi

Research Institute for Applied Mechanics, Kyushu University

M

Mei-Yi Fan

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

F

Feng Xie

Z

Zhu-Yu Zhao

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

M

Mingyuan Yu

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

F

Fang Cao

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

R

Rongshuang Xu

Jiangsu Key Laborartory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, Joint International Research Laboratory of Climate and Environment Change, School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology

J

Jianghanyang Li

Institute of Arctic and Alpine Research, University of Colorado

K

Kimitaka Kawamura

Chubu Institute for Advanced Study, Chubu University

M

Mark H. Thiemens

Department of Chemistry and Biochemistry, University of California