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Stratospheric CH4, HCl and ClO and the chlorine-ozone cycle

dc.contributor.authorAckerman, M.
dc.contributor.authorFrimout, D.
dc.contributor.authorMuller, C.
dc.date1977
dc.date.accessioned2017-09-05T10:19:17Z
dc.date.available2017-09-05T10:19:17Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/6141
dc.descriptionSINCE it was suggested1 that chlorine may influence stratospheric ozone balance, and that halocarbons can contribute significantly to the stratospheric chlorine content2-4 much attention has been paid to the subject. We report here a new determination of atmospheric methane levels which gives a value lower than that often assumed by other workers. In model calculations this suggests that chlorine has a greater effect on the ozone balance than previously suspected.
dc.languageeng
dc.titleStratospheric CH4, HCl and ClO and the chlorine-ozone cycle
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freechlorine
dc.subject.freemethane
dc.subject.freeozone
dc.subject.freemethodology
dc.subject.freestratosphere
dc.source.titleNature
dc.source.volume269
dc.source.issue5625
dc.source.page226-227
Orfeo.peerreviewedYes
dc.identifier.doi10.1038/269226a0
dc.identifier.scopus2-s2.0-0017757231


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