Long‐term temperature trends in the stratosphere: Possible influence of anthropogenic gases

dc.contributor.author	Labitzke, K.
dc.contributor.author	Brasseur, G.
dc.contributor.author	Naujokat, B.
dc.contributor.author	De Rudder, A.
dc.date	1986
dc.date.accessioned	2017-06-16T11:51:53Z
dc.date.available	2017-06-16T11:51:53Z
dc.identifier.uri	https://orfeo.belnet.be/handle/internal/5832
dc.description	Analysis 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.language	eng
dc.title	Long‐term temperature trends in the stratosphere: Possible influence of anthropogenic gases
dc.type	Article
dc.subject.frascati	Physical sciences
dc.audience	Scientific
dc.source.title	Geophysical Research Letters
dc.source.volume	13
dc.source.issue	1
dc.source.page	52-55
Orfeo.peerreviewed	Yes
dc.identifier.doi	10.1029/GL013i001p00052
dc.identifier.scopus	2-s2.0-0022835592