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dc.contributor.authorDemoulin, P.
dc.contributor.authorZander, R.
dc.contributor.authorMahieu, E.
dc.contributor.authorRinsland, C.P.
dc.contributor.authorPugachev, N.
dc.contributor.authorNewport, C.
dc.contributor.authorDe Mazière, M.
dc.contributor.authorHennen, O.
dc.contributor.authorBarbe, A.
dc.date1995
dc.date.accessioned2023-03-30T11:04:41Z
dc.date.available2023-03-30T11:04:41Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/10848
dc.descriptionWe have attempted to discriminate between tropospheric and stratospheric burdens of ozone making up the total columns routinely derived above the Jungfraujoch from the spectral analysis of isolated lines. For that, we have identified a number of spectral intervals containing multiple ozone transitions in which the central core of the line and the throughs between these are predominantly sensitive to, respectively, the stratospheric and lower tropospheric contents of ozone. A realistic initial volume mixing ratio profile of ozone is progressively adjusted over various layers until the root square sum of the residuals of the fit to the observations reaches a minimum. The role of the observational geometry in improving the tropospheric/stratospheric O3 ratio is also being investigated.
dc.languageeng
dc.titleTotal ozone monitoring above the Jungfraujoch by FTIR relative tropospheric and stratospheric contributions
dc.typeConference
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeozone
dc.subject.freeatmospheric composition
dc.subject.freeinfrared spectroscopy
dc.subject.freetroposphere
dc.subject.freestratosphere
dc.subject.freeFTIR
dc.subject.freeJungfraujoch
dc.source.titleInternational conference on ozone in the lower stratosphere, Halkidiki, Greece, May 15-20, 1995
dc.source.page21-22
Orfeo.peerreviewedNo
dc.identifier.scopus


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