Show simple item record

dc.contributor.authorSioris, C.E.
dc.contributor.authorChabrillat, S.
dc.contributor.authorMcLinden, C.A.
dc.contributor.authorHaley, C.S.
dc.contributor.authorRochon, Y.J.
dc.contributor.authorMénard, R.
dc.contributor.authorCharron, M.
dc.contributor.authorMcElroy, C.T.
dc.date2007
dc.date.accessioned2016-09-27T11:09:46Z
dc.date.available2016-09-27T11:09:46Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/4398
dc.descriptionSelected NOx profiles of the Antarctic lower stratosphere inferred from OSIRIS NO2 observations are presented from the austral spring of 2003. These observations show a tongue of NOx at 100 hPa, with a concentration typical of the middle stratosphere. Simulations with the Global Environmental Multiscale model show that this small-scale tongue of NOx-rich air descended into the lower stratosphere. The tongue was formed as a result of a Rossby wave breaking days earlier, transporting NO x from the pole, where larger concentrations had recently appeared, to the edge of the vortex. The three-dimensional structure of the breaking wave is illustrated in detail.
dc.languageeng
dc.relation.ispartofseries
dc.titleOSIRIS observations of a tongue of NOx in the lower stratosphere at the Antarctic vortex edge: Comparison with a high-resolution simulation from the Global Environmental Multiscale (GEM) model
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.subject.freeComputer simulation
dc.subject.freeMathematical models
dc.subject.freeNitrogen compounds
dc.subject.freeUpper atmosphere
dc.subject.freeAustral spring
dc.subject.freeGlobal Environmental Multiscale (GEM) model
dc.subject.freeInfrared imaging
dc.source.titleCanadian Journal of Physics
dc.source.volume85
dc.source.issue11
dc.source.page1195-1207
Orfeo.peerreviewedYes
dc.identifier.doi10.1139/P07-123
dc.identifier.scopus2-s2.0-38849115168


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record