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dc.contributor.authorBates, D.R.
dc.contributor.authorNicolet, M.
dc.date1965
dc.date.accessioned2017-08-18T10:22:57Z
dc.date.available2017-08-18T10:22:57Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5960
dc.descriptionAttention is drawn to the possibility that H + HO2 → H2 + O2 may be an important source of hydrogen molecules in the lower thermosphere. It is suggested that the fractional volume abundance of hydrogen atoms (free and combined) in this region is determined by, and is not very much less than, the corresponding fractional volume abundance in the stratosphere. Any hydrogen molecules in the lower thermosphere would affect the altitude distribution of hydrogen atoms and augment their rate of escape.
dc.languageeng
dc.titleAtmospheric hydrogen
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.source.titlePlanetary and Space Science
dc.source.volume13
dc.source.issue9
dc.source.page905-909
Orfeo.peerreviewedYes
dc.identifier.doi10.1016/0032-0633(65)90175-3
dc.identifier.scopus2-s2.0-0007411142


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