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dc.contributor.authorAckerman, M.
dc.date1974
dc.date.accessioned2017-08-30T13:27:26Z
dc.date.available2017-08-30T13:27:26Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/6048
dc.descriptionA volume of mixing ratio equal to (3·4 ± 0.7) × 10-6 is deduced for the stratospheric water vapour from 20 to 37 km. The results have been obtained by absorptiometry from a balloon platform at 40 km.
dc.languageeng
dc.titleStratospheric water vapor from high resolution infrared spectra
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.source.titlePlanetary and Space Science
dc.source.volume22
dc.source.issue8
dc.source.page1265-1267
Orfeo.peerreviewedYes
dc.identifier.doi10.1016/0032-0633(74)90009-9
dc.identifier.scopus2-s2.0-49549158877


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