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dc.contributor.authorBrasseur, G.
dc.contributor.authorDe Rudder, A.
dc.date1987
dc.date.accessioned2017-06-13T09:35:56Z
dc.date.available2017-06-13T09:35:56Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5806
dc.descriptionThe response of the atmosphere to emissions of chlorofluorocarbons (CFCs) and other chlorocarbons and to increasing concentrations of other radiatively active trace gases is calculated by means of a coupled chemical-radiative-transport one-dimensional model. It is shown that significant reductions in the ozone concentration and in the temperature should be expected in the upper stratosphere as a result essentially of increasing concentrations of active chlorine produced by photodecomposition of the CFCs.
dc.languageeng
dc.titleThe potential impact on atmospheric ozone and temperature of increasing trace gas concentrations
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.source.titleJournal of Geophysical Research
dc.source.volume92
dc.source.issueD9
dc.source.page10903-10920
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/JD092iD09p10903
dc.identifier.scopus2-s2.0-0023520557


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