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dc.contributor.authorAckerman, M.
dc.contributor.authorFrimout, D.
dc.contributor.authorGirard, A.
dc.contributor.authorGottignies, M.
dc.contributor.authorMuller, C.
dc.date1976
dc.date.accessioned2017-09-01T12:11:13Z
dc.date.available2017-09-01T12:11:13Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/6101
dc.descriptionHCl has been observed in the stratosphere from balloon borne spectroscopic measurements of a portion of the fundamental band in the 3 microns wavelength region. The observation of absorption lines using the sun as a source at solar zenith angles larger than 90° indicates an HCl volume mixing ratio equal to (3.8 ± 1.5) × 10−10 at 20 km increasing with altitude at least up to 30 km where the value is (1.4 ± 0.6) × 10−9. The total zenith amount above 21 km is found to be (10± 3.5) × 10−14 cm−2 in agreement with previous observations performed up to this altitude. A maximum number density equal to (7.2 ± 3) × 108 cm−3 is observed at 24 ± 2 km altitude.
dc.languageeng
dc.titleStratospheric HCl from infrared spectra
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.source.titleGeophysical Research Letters
dc.source.volume3
dc.source.issue2
dc.source.page81-83
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/GL003i002p00081
dc.identifier.scopus2-s2.0-1642472289


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