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dc.contributor.authorLabitzke, K.
dc.contributor.authorBrasseur, G.
dc.contributor.authorNaujokat, B.
dc.contributor.authorDe Rudder, A.
dc.date1986
dc.date.accessioned2017-06-16T11:51:53Z
dc.date.available2017-06-16T11:51:53Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5832
dc.descriptionAnalysis of northern hemisphere mid‐latitude temperature data at 30 mbar over the last 20 years suggests a long‐term negative trend of about ‐0.24 K/decade when all observations between 10°N and 90°N are considered. This stratospheric cooling which could tentatively be attributed to the increase of the carbon dioxide amount in the stratosphere is in qualitative agreement at 30 mbar with a model calculation of the historical evolution of temperature and chemical composition in the middle atmosphere.
dc.languageeng
dc.titleLong‐term temperature trends in the stratosphere: Possible influence of anthropogenic gases
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.source.titleGeophysical Research Letters
dc.source.volume13
dc.source.issue1
dc.source.page52-55
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/GL013i001p00052
dc.identifier.scopus2-s2.0-0022835592


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