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dc.contributor.authorAchard, V.
dc.contributor.authorDe Mazière, M.
dc.contributor.authorCamy-Peyret, C.
dc.contributor.authorKarcher, F.
dc.contributor.authorLippens, C.
dc.date1997
dc.date.accessioned2017-05-22T13:18:39Z
dc.date.available2017-05-22T13:18:39Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5475
dc.descriptionThe GRILLE infrared spectrometer was part of the shuttle payload during the first ATLAS mission in March-April 1992. This experiment measured the vertical distribution of several important minor constituents in the middle to high atmosphere by solar occultation mid-infrared absorption spectroscopy. Among the molecules observed is the stratospheric chlorine reservoir species HCl. This paper discusses the vertical profiles measured, including their validation with respect to correlative measurements from ATMOS on board the same mission and from HALOE on board UARS. The most 1 important conclusion drawn from the measured HCl volume mixing ratio of (3.6±0.2) ppbv above 50 km presently measured by GRILLE in comparison with published ATMOS data from 1985 is that the actual GRILLE data confirm the increase of the upper stratospheric total chlorine loading by about 40% with respect to 1985, as reported and/or predicted earlier.
dc.languageeng
dc.titleSpaceborne measurements of the upper stratospheric HCL vertical distribution in early 1992 and the trend in total stratospheric chlorine since 1985
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeATMOS
dc.subject.freeatmospheric chemistry
dc.subject.freechlorine
dc.subject.freeHALOE
dc.subject.freehydrogen chlorine
dc.subject.freesatellite measurement
dc.subject.freespectrometer
dc.subject.freestratosphere
dc.subject.freeUARS
dc.source.titleJournal of Geophysical Research Atmospheres
dc.source.volume102
dc.source.issue7
dc.source.page8985-8990
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/97JD00004
dc.identifier.scopus2-s2.0-0031416452


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