Quantifying contributions of chlorofluorocarbon banks to emissions and impacts on the ozone layer and climate

Chlorofluorocarbon (CFC) banks from uses such as air conditioners or foams can be emitted after global production stops. Recent reports of unexpected emissions of CFC-11 raise the need to better quantify releases from these banks, and associated impacts on ozone depletion and climate change. Here we...

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Bibliographic Details
Main Authors: Lickley, Megan Jeramaz (Author), Solomon, Susan (Author), Fletcher, Sarah Marie (Author), Stone, Kane Adam (Author)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor), Massachusetts Institute of Technology. Department of Civil and Environmental Engineering (Contributor)
Format: Article
Language:English
Published: Springer Science and Business Media LLC, 2020-04-15T19:38:12Z.
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Online Access:Get fulltext
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100 1 0 |a Lickley, Megan Jeramaz  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences  |e contributor 
100 1 0 |a Massachusetts Institute of Technology. Department of Civil and Environmental Engineering  |e contributor 
700 1 0 |a Solomon, Susan  |e author 
700 1 0 |a Fletcher, Sarah Marie  |e author 
700 1 0 |a Stone, Kane Adam  |e author 
245 0 0 |a Quantifying contributions of chlorofluorocarbon banks to emissions and impacts on the ozone layer and climate 
260 |b Springer Science and Business Media LLC,   |c 2020-04-15T19:38:12Z. 
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520 |a Chlorofluorocarbon (CFC) banks from uses such as air conditioners or foams can be emitted after global production stops. Recent reports of unexpected emissions of CFC-11 raise the need to better quantify releases from these banks, and associated impacts on ozone depletion and climate change. Here we develop a Bayesian probabilistic model for CFC-11, 12, and 113 banks and their emissions, incorporating the broadest range of constraints to date. We find that bank sizes of CFC-11 and CFC-12 are larger than recent international scientific assessments suggested, and can account for much of current estimated CFC-11 and 12 emissions (with the exception of increased CFC-11 emissions after 2012). Left unrecovered, these CFC banks could delay Antarctic ozone hole recovery by about six years and contribute 9 billion metric tonnes of equivalent CO2 emission. Derived CFC-113 emissions are subject to uncertainty, but are much larger than expected, raising questions about its sources. ©2020 
546 |a en 
655 7 |a Article 
773 |t 10.1038/s41467-020-15162-7 
773 |t Nature communications