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dc.contributor.authorKinnison, Doug
dc.contributor.authorMills, Michael J.
dc.contributor.authorNeely, Ryan R.
dc.contributor.authorSchmidt, Anja
dc.contributor.authorSolomon, Susan
dc.contributor.authorIvy, Diane J
dc.date.accessioned2017-03-06T20:00:41Z
dc.date.available2017-03-06T20:00:41Z
dc.date.issued2016-07
dc.date.submitted2015-12
dc.identifier.issn0036-8075
dc.identifier.issn1095-9203
dc.identifier.urihttp://hdl.handle.net/1721.1/107197
dc.description.abstractIndustrial chlorofluorocarbons that cause ozone depletion have been phased out under the Montreal Protocol. A chemically driven increase in polar ozone (or “healing”) is expected in response to this historic agreement. Observations and model calculations together indicate that healing of the Antarctic ozone layer has now begun to occur during the month of September. Fingerprints of September healing since 2000 include (i) increases in ozone column amounts, (ii) changes in the vertical profile of ozone concentration, and (iii) decreases in the areal extent of the ozone hole. Along with chemistry, dynamical and temperature changes have contributed to the healing but could represent feedbacks to chemistry. Volcanic eruptions have episodically interfered with healing, particularly during 2015, when a record October ozone hole occurred after the Calbuco eruption.en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (FESD Grant OCE-1338814)en_US
dc.description.sponsorshipNational Science Foundation (U.S.). Atmospheric Chemistry Program (Grant 1539972)en_US
dc.language.isoen_US
dc.publisherAmerican Association for the Advancement of Scienceen_US
dc.relation.isversionofhttp://dx.doi.org/10.1126/science.aae0061en_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.sourceMIT Web Domainen_US
dc.titleEmergence of healing in the Antarctic ozone layeren_US
dc.typeArticleen_US
dc.identifier.citationSolomon, Susan et al. “Emergence of Healing in the Antarctic Ozone Layer.” Science 353.6296 (2016): 269–274.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorSolomon, Susan
dc.contributor.mitauthorIvy, Diane J
dc.relation.journalScienceen_US
dc.eprint.versionAuthor's final manuscripten_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsSolomon, Susan; Ivy, Diane J.; Kinnison, Doug; Mills, Michael J.; Neely, Ryan R.; Schmidt, Anjaen_US
dspace.embargo.termsNen_US
dc.identifier.orcidhttps://orcid.org/0000-0002-2020-7581
mit.licensePUBLISHER_POLICYen_US


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