Several notes on the OH* layer

dc.bibliographicCitation.firstPage	923	eng
dc.bibliographicCitation.issue	7	eng
dc.bibliographicCitation.journalTitle	Annales geophysicae	eng
dc.bibliographicCitation.lastPage	930	eng
dc.bibliographicCitation.volume	33	eng
dc.contributor.author	Grygalashvyly, M.
dc.date.accessioned	2022-06-23T11:50:23Z
dc.date.available	2022-06-23T11:50:23Z
dc.date.issued	2015
dc.description.abstract	This brief note introduces several analytical approaches to OH* layer parameters. The number density and height of the OH* layer peak are determined by the distributions of atomic oxygen and temperature, and by corresponding vertical gradients. The theory can be applied to satellite-borne and ground-based airglow measurements, as well as to model results.	eng
dc.description.version	publishedVersion	eng
dc.identifier.uri	https://oa.tib.eu/renate/handle/123456789/9175
dc.identifier.uri	https://doi.org/10.34657/8213
dc.language.iso	eng	eng
dc.publisher	Katlenburg, Lindau : Copernicus	eng
dc.relation.doi	https://doi.org/10.5194/angeo-33-923-2015
dc.relation.essn	1432-0576
dc.rights.license	CC BY 3.0 Unported	eng
dc.rights.uri	https://creativecommons.org/licenses/by/3.0/	eng
dc.subject.ddc	550	eng
dc.subject.other	Atmospheric composition and structure (airglow and aurora; middle atmosphere - composition and chemistry; thermosphere-composition and chemistry)	eng
dc.title	Several notes on the OH* layer	eng
dc.type	Article	eng
dc.type	Text	eng
tib.accessRights	openAccess	eng
wgl.contributor	IAP	eng
wgl.subject	Geowissenschaften	eng
wgl.type	Zeitschriftenartikel	eng

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