Substantial increase in perfluorocarbons CF 4 (PFC-14) and C 2 F 6 (PFC-116) emissions in China

Author:

An Minde123ORCID,Prinn Ronald G.1ORCID,Western Luke M.3ORCID,Yao Bo456ORCID,Zhao Xingchen2,Kim Jooil7ORCID,Mühle Jens7ORCID,Chi Wenxue5,Harth Christina M.7ORCID,Hu Jianxin2ORCID,Ganesan Anita L.18ORCID,Rigby Matthew13ORCID

Affiliation:

1. Center for Global Change Science, Massachusetts Institute of Technology, Cambridge, MA 02139

2. College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China

3. School of Chemistry, University of Bristol, Bristol BS8 1TS, United Kingdom

4. Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences, Fudan University, Shanghai 200438, China

5. Meteorological Observation Centre of China Meteorological Administration, Beijing 100081, China

6. Shanghai Key Laboratory of Ocean-land-atmosphere Boundary Dynamics and Climate Change, Shanghai 200438, China

7. Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093

8. School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, United Kingdom

Abstract

The perfluorocarbons tetrafluoromethane (CF 4 , PFC-14) and hexafluoroethane (C 2 F 6 , PFC-116) are potent greenhouse gases with near-permanent atmospheric lifetimes relative to human timescales and global warming potentials thousands of times that of CO 2 . Using long-term atmospheric observations from a Chinese network and an inverse modeling approach (top–down method), we determined that CF 4 emissions in China increased from 4.7 (4.2-5.0, 68% uncertainty interval) Gg y −1 in 2012 to 8.3 (7.7-8.9) Gg y −1 in 2021, and C 2 F 6 emissions in China increased from 0.74 (0.66-0.80) Gg y −1 in 2011 to 1.32 (1.24-1.40) Gg y −1 in 2021, both increasing by approximately 78%. Combined emissions of CF 4 and C 2 F 6 in China reached 78 Mt CO 2 -eq in 2021. The absolute increase in emissions of each substance in China between 2011-2012 and 2017-2020 was similar to (for CF 4 ), or greater than (for C 2 F 6 ), the respective absolute increase in global emissions over the same period. Substantial CF 4 and C 2 F 6 emissions were identified in the less-populated western regions of China, probably due to emissions from the expanding aluminum industry in these resource-intensive regions. It is likely that the aluminum industry dominates CF 4 emissions in China, while the aluminum and semiconductor industries both contribute to C 2 F 6 emissions. Based on atmospheric observations, this study validates the emission magnitudes reported in national bottom–up inventories and provides insights into detailed spatial distributions and emission sources beyond what is reported in national bottom–up inventories.

Publisher

Proceedings of the National Academy of Sciences

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