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 |