Stable chloroform emissions in southeastern China: insights from recent observations.

Authors

Zhiwei Cao, Yonglong Lu, Pei Wang, Yunlei Zhang, Yulin Xu, Zhaoyang Wu, Xinyi Huang, Haojie Lei, Bin Sun, Jialong Li, Xudong Jiang, Yizhou Jiang

Published in

Journal of environmental sciences (China). Volume 168. Pages 504-511. Epub Jan 13, 2026.

Abstract

Chloroform (CHCl₃) is a short-lived ozone-depleting substance not currently regulated under the Montreal Protocol. Due to the unique meteorological conditions in East Asia, CHCl₃ emitted in this region has a greater potential to reach the stratosphere and contribute to ozone depletion. As an essential component of national CHCl₃ emissions, southeastern China has attracted increasing attention. However, long-term observational data in this region remain relatively scarce, with no updates since 2020. In this study, we continuously measured atmospheric CHCl₃ concentrations at a remote monitoring station in southeastern China from 1 June 2023 to 31 May 2025. Frequent concentration enhancements were observed during the monitoring period, with mixing ratios ranging from 9.3 to 134.1 ppt and an average value of 36.8 ± 19.7 ppt. Back-trajectory analysis indicated that air masses associated with elevated CHCl₃ levels primarily originated from coastal industrial provinces in eastern China. Using the Potential Source Contribution Function and Concentration Weighted Trajectory methods, we identified the Yangtze River Delta (Jiangsu, Anhui, and Zhejiang Provinces) and Jiangxi Province as dominant source regions. Emissions of CHCl₃ in southeastern China were estimated using the Tracer Ratio Method to be approximately 30.1 ± 5.3 Gg/yr from 2023-06-01 to 2025-05-31, indicating overall stability relative to earlier estimates and no apparent upward trend. These findings provide updated insights into the current status of CHCl₃ emissions in southeastern China and highlight the need for continued monitoring and emission assessment of CHCl₃ in East Asia, given its unregulated status and implications for ozone layer recovery.

PMID:
42680408
Bibliographic data and abstract were imported from PubMed on 02 Sep 2026.

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