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dc.contributor.authorBrasseur, G.
dc.contributor.authorHitchman, M.H.
dc.contributor.authorSimon, P.C.
dc.contributor.authorDe Rudder, A.
dc.date1988
dc.date.accessioned2017-06-08T12:20:53Z
dc.date.available2017-06-08T12:20:53Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5767
dc.descriptionAn interpretation of global ozone changes deduced from satellite data obtained since 1979 is presented, based on two‐dimensional model simulations. The study shows that a depletion in total ozone of the order of 2 percent and a reduction in ozone density near 40 km of 7 to 12 percent over the 1979–1986 period are consistent with the observed increase in trace gas densities (chlorofluorocarbons, methane, nitrous oxide, carbon dioxide) and the simultaneous decrease in solar activity during this period. The model also suggests that ozone variations of solar and anthropogenic origins between 1979 and 1986 were of similar magnitude but that the ozone response to trace gas emissions increases substantially with latitude while the solar signal in ozone is present lower in the atmosphere and is nearly independent of latitude.
dc.languageeng
dc.titleOzone reduction in the 1980's: A model simulation of anthropogenic and solar perturbations
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeanthropogenic perturbation
dc.subject.freecarbon dioxide
dc.subject.freechlorofluorocarbon
dc.subject.freemethane
dc.subject.freenitrous oxide
dc.subject.freeozone reduction
dc.subject.freesolar perturbation
dc.subject.freetrace gas
dc.source.titleGeophysical Research Letters
dc.source.volume15
dc.source.issue12
dc.source.page1361-1364
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/GL015i012p01361
dc.identifier.scopus2-s2.0-0024194932


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