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dc.contributor.authorO'Doherty, Simon
dc.contributor.authorMiller, Benjamin R.
dc.contributor.authorHarth, C. M.
dc.contributor.authorSalameh, P. K.
dc.contributor.authorArnold, T.
dc.contributor.authorWeiss, R. F.
dc.contributor.authorKrummel, P. B.
dc.contributor.authorSteele, L. P.
dc.contributor.authorFraser, P. J.
dc.contributor.authorYoung, D.
dc.contributor.authorSimmonds, P. G.
dc.contributor.authorRigby, Matthew
dc.contributor.authorMuhle, Jens
dc.contributor.authorPrinn, Ronald G
dc.contributor.authorIvy, Diane J
dc.date.accessioned2015-10-06T17:28:31Z
dc.date.available2015-10-06T17:28:31Z
dc.date.issued2014-04
dc.date.submitted2013-12
dc.identifier.issn00948276
dc.identifier.urihttp://hdl.handle.net/1721.1/99158
dc.description.abstractAtmospheric measurements show that emissions of hydrofluorocarbons (HFCs) and hydrochlorofluorocarbons are now the primary drivers of the positive growth in synthetic greenhouse gas (SGHG) radiative forcing. We infer recent SGHG emissions and examine the impact of future emissions scenarios, with a particular focus on proposals to reduce HFC use under the Montreal Protocol. If these proposals are implemented, overall SGHG radiative forcing could peak at around 355 mW m[superscript −2] in 2020, before declining by approximately 26% by 2050, despite continued growth of fully fluorinated greenhouse gas emissions. Compared to “no HFC policy” projections, this amounts to a reduction in radiative forcing of between 50 and 240 mW m[superscript −2] by 2050 or a cumulative emissions saving equivalent to 0.5 to 2.8 years of CO2 emissions at current levels. However, more complete reporting of global HFC emissions is required, as less than half of global emissions are currently accounted for.en_US
dc.description.sponsorshipNatural Environment Research Council (Great Britain) (Advanced Research Fellowship NE/I021365/1)en_US
dc.description.sponsorshipUnited States. National Aeronautics and Space Administration (Upper Atmospheric Research Program Grant NNX11AF17G)en_US
dc.description.sponsorshipUnited States. National Oceanic and Atmospheric Administrationen_US
dc.language.isoen_US
dc.publisherWiley Blackwellen_US
dc.relation.isversionofhttp://dx.doi.org/10.1002/2013gl059099en_US
dc.rightsArticle is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.en_US
dc.sourceProf. Prinn via Chris Sherratten_US
dc.titleRecent and future trends in synthetic greenhouse gas radiative forcingen_US
dc.typeArticleen_US
dc.identifier.citationRigby, M., R. G. Prinn, S. O’Doherty, B. R. Miller, D. Ivy, J. Muhle, C. M. Harth, et al. “Recent and Future Trends in Synthetic Greenhouse Gas Radiative Forcing.” Geophysical Research Letters 41, no. 7 (April 4, 2014): 2623–2630. © 2014 American Geophysical Unionen_US
dc.contributor.departmentMassachusetts Institute of Technology. Center for Global Change Scienceen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.approverPrinn, Ronald G.en_US
dc.contributor.mitauthorRigby, Matthewen_US
dc.contributor.mitauthorPrinn, Ronald G.en_US
dc.contributor.mitauthorIvy, Diane J.en_US
dc.relation.journalGeophysical Research Lettersen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsRigby, M.; Prinn, R. G.; O'Doherty, S.; Miller, B. R.; Ivy, D.; Muhle, J.; Harth, C. M.; Salameh, P. K.; Arnold, T.; Weiss, R. F.; Krummel, P. B.; Steele, L. P.; Fraser, P. J.; Young, D.; Simmonds, P. G.en_US
dc.identifier.orcidhttps://orcid.org/0000-0001-5925-3801
mit.licensePUBLISHER_POLICYen_US
mit.metadata.statusComplete


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