Vibration-rotation spectrum of CIO and its role in the stratosphere

Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/4767

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DC Field	Value	Language
dc.contributor.author	Murty, P. S	-
dc.date.accessioned	2009-08-28T14:20:29Z	-
dc.date.available	2009-08-28T14:20:29Z	-
dc.date.issued	1979-10	-
dc.identifier.citation	Journal of the Atmospheric Sciences, Vol. 36, No. 10, pp. 2026 – 2028	en
dc.identifier.issn	0022-4928	-
dc.identifier.uri	http://hdl.handle.net/2248/4767	-
dc.description.abstract	The possible role in the stratosphere of vibrationally excited chlorine monoxide molecules in the ground electronic state is examined. An infrared vibration-rotation emission spectrum of chlorine monoxide is expected to arise following the neutral rearrangement reaction between atomic chlorine and ozone. The predicted vibration-rotation spectrum in the 676.75–4897.81 cm−1 region is described.	en
dc.language.iso	en	en
dc.publisher	American Meteorological Society	en
dc.relation.uri	http://dx.doi.org/10.1175/1520-0469	en
dc.rights	© American Meteorological Society	en
dc.subject	Vibration Rotation Spectrum	en
dc.subject	Stratosphere	en
dc.title	Vibration-rotation spectrum of CIO and its role in the stratosphere	en
dc.type	Article	en
Appears in Collections:	IIAP Publications

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