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dc.contributor.authorVandaele, A.C.
dc.contributor.authorDe Mazière, M.
dc.contributor.authorDrummond, R.
dc.contributor.authorMahieux, A.
dc.contributor.authorNeefs, E.
dc.contributor.authorWilquet, V.
dc.contributor.authorKorablev, O.
dc.contributor.authorFedorova, A.
dc.contributor.authorBelyaev, D.
dc.contributor.authorMontmessin, F.
dc.contributor.authorBertaux, J.-L.
dc.date2008
dc.date.accessioned2016-09-21T10:35:07Z
dc.date.available2016-09-21T10:35:07Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/4316
dc.descriptionSolar Occultation at Infrared (SOIR), which is a part of the Spectroscopy for Investigation of Characteristics of the Atmosphere of Venus (SPICAV) instrument on board Venus Express, combines an echelle-grating spectrometer with an acoustooptical tunable filter. It performs solar occultation measurements in the IR region at a high spectral resolution better than all previously flown planetary spectrometers. The wavelength range probed allows for a detailed chemical inventory of the Venus atmosphere above the cloud layer, with an emphasis on the vertical distribution of the gases. A general description of the retrieval technique is given and is illustrated by some results obtained for CO2 and for a series of minor constituents, such as H2O, HDO, CO, HCl, and HF. Detection limits for previously undetected species will also be discussed.
dc.languageeng
dc.titleComposition of the Venus mesosphere measured by Solar Occultation at Infrared on board Venus Express
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.source.titleJournal of Geophysical Research E: Planets
dc.source.volume113
dc.source.issue5
dc.source.pageE00B23
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/2008JE003140
dc.identifier.scopus2-s2.0-77952258919


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