Semi-empirical estimates of stratospheric circulation and the lifetimes of chlorofluorocarbons and carbon tetrachloride

Abstract Chlorofluorocarbons (CFCs) and carbon tetrachloride (CCl 4 ) are ozone-depleting substances with high radiative efficiencies; however, uncertainties in their atmospheric lifetimes hinder top-down emission monitoring efforts. Here, we compute the loss, emission, and lifetime of CFC-11, CFC-12, and CCl 4 using their mass balance in the stratosphere. We first infer the strength of the stratospheric overturning circulation using satellite measurements of nitrous oxide; the mass flux at about 18 km is then used to compute the loss of CFC-11, CFC-12, and CCl 4 . We confirm that anomalous surface measurements of CFC-11 from 2013 to 2018 cannot be attributed to variability in stratospheric transport alone, and we infer near-steady CCl 4 emissions since 2013. Atmospheric lifetimes (50, 86, and 41 yr) independent of previous work are also computed using loss rates. These estimates add confidence to emission inversions and projections of the compounds’ ozone and climate impacts, and may help detect breaches of the Montreal Protocol.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-07-05
DOI
https://doi.org/10.1038/s43247-025-02500-0
Citations
1
Primary Topic
Atmospheric Ozone and Climate
Type
article
Field-Weighted Citation Impact
1.30

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article

Semi-empirical estimates of stratospheric circulation and the lifetimes of chlorofluorocarbons and carbon tetrachloride

Stephen Bourguet, Kane A. Stone, Megan Lickley
1 citations
Communications Earth & Environment
Atmospheric Ozone and Climate
1.30
article

Semi-empirical estimates of stratospheric circulation and the lifetimes of chlorofluorocarbons and carbon tetrachloride

Stephen Bourguet, Kane A. Stone, Megan Lickley
article en
1 citations

Abstract

Abstract Chlorofluorocarbons (CFCs) and carbon tetrachloride (CCl 4 ) are ozone-depleting substances with high radiative efficiencies; however, uncertainties in their atmospheric lifetimes hinder top-down emission monitoring efforts. Here, we compute the loss, emission, and lifetime of CFC-11, CFC-12, and CCl 4 using their mass balance in the stratosphere. We first infer the strength of the stratospheric overturning circulation using satellite measurements of nitrous oxide; the mass flux at about 18 km is then used to compute the loss of CFC-11, CFC-12, and CCl 4 . We confirm that anomalous surface measurements of CFC-11 from 2013 to 2018 cannot be attributed to variability in stratospheric transport alone, and we infer near-steady CCl 4 emissions since 2013. Atmospheric lifetimes (50, 86, and 41 yr) independent of previous work are also computed using loss rates. These estimates add confidence to emission inversions and projections of the compounds’ ozone and climate impacts, and may help detect breaches of the Montreal Protocol.

Communications Earth & EnvironmentVol. 6(1)
Georgetown University (US), Massachusetts Institute of Technology (US)
National Science Foundation, U.S. Department of Energy, National Aeronautics and Space Administration, Massachusetts Institute of Technology, University of Bristol, Commonwealth Scientific and Industrial Research Organisation, Nuclear Safety and Security Commission, Miljødirektoratet, National Oceanic and Atmospheric Administration, Bundesamt für Umwelt
Openalex Percentile: Top 21%
Atmospheric Ozone and Climate
1.30
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