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dc.contributor.authorHauchecorne, A.
dc.contributor.authorBertaux, J.-L.
dc.contributor.authorDalaudier, F.
dc.contributor.authorRussell, J.M.
dc.contributor.authorMlynczak, M.G.
dc.contributor.authorKyrölä, E.
dc.contributor.authorFussen, D.
dc.date2007
dc.date.accessioned2016-09-26T12:43:58Z
dc.date.available2016-09-26T12:43:58Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/4371
dc.descriptionOdd nitrogen species play an important role in the stratospheric ozone balance through catalytic ozone destruction. A layer of strongly enhanced NO2 was detected in the north polar mesosphere by the GOMOS/ENVISAT stellar spectrometer in mid-January 2004. Large NO2 enhancements in the polar winter mesosphere have been previously reported by several authors and have been attributed to NO production by solar proton or by energetic electron precipitations. The simultaneous occurrence of an intense mesospheric warming observed by the SABER/TIMED instrument indicates that a strong air descent occurred in the polar region, transporting a large quantity of NO from the upper mesosphere-lower thermosphere to the lower mesosphere. The proposed mechanism may have a significant contribution to the budget of polar stratospheric ozone.
dc.languageeng
dc.relation.ispartofseries
dc.titleLarge increase of NO2 in the north polar mesosphere in January-February 2004: Evidence of a dynamical origin from GOMOS/ENVISAT and SABER/TIMED data
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeAtmospheric chemistry
dc.subject.freeAtmospheric composition
dc.subject.freeOzone
dc.subject.freeSatellite imagery
dc.subject.freeUpper atmosphere
dc.subject.freeEnergetic electron precipitation
dc.subject.freeSolar proton
dc.subject.freeStratospheric ozone
dc.subject.freeGeophysics
dc.subject.freeEnvisat-1
dc.subject.freemesosphere
dc.subject.freenitrogen dioxide
dc.subject.freepolar region
dc.subject.freeremote sensing
dc.source.titleGeophysical Research Letters
dc.source.volume34
dc.source.issue3
dc.source.pageL03810
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/2006GL027628
dc.identifier.scopus2-s2.0-34548016306


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