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dc.contributor.authorFussen, D.
dc.contributor.authorVanhellemont, F.
dc.contributor.authorBingen, C.
dc.contributor.authorChabrillat, S.
dc.date2000
dc.date.accessioned2017-09-04T09:03:43Z
dc.date.available2017-09-04T09:03:43Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/6118
dc.descriptionWe present ozone volume mixing ratio profiles obtained by the ORA instrument during the period Aug 1992-Apr 1993. They have been retrieved by applying a specific inversion algorithm to a radiometric UV channel contaminated by Rayleigh scattering. The results compare reasonably well with other instruments up to the mesopause and are probably the first extended ozone data in the lower thermosphere (90-110 km).
dc.languageeng
dc.titleOzone profiles from 30 to 110 km measured by the occultation radiometer instrument during the period Aug 1992-Apr 1993
dc.typeArticle
dc.audienceScientific
dc.subject.freeinstrumentation
dc.subject.freeozone
dc.subject.freeAlgorithms
dc.subject.freeOzone
dc.subject.freeRadiometers
dc.subject.freeRayleigh scattering
dc.subject.freeRemote sensing
dc.subject.freeUltraviolet instruments
dc.subject.freeInversion algorithms
dc.subject.freeOccultation radiometers
dc.subject.freeThermosphere
dc.subject.freeAtmospheric composition
dc.source.titleGeophysical Research Letters
dc.source.volume27
dc.source.issue21
dc.source.page3449-3452
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/2000GL011575
dc.identifier.scopus2-s2.0-0034352501


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