Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38096
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dc.contributor.authorSrivastava, A. N.-
dc.contributor.authorSrivastava, R. D.-
dc.date.accessioned2016-12-02T09:13:14Z-
dc.date.available2016-12-02T09:13:14Z-
dc.date.issued1972-12-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38096-
dc.description241-243en_US
dc.description.abstractAn analysis if the experimental results on absorption of ultraviolet radiation by atmospheric gases indicates that the absorption processes obey spin conservation rule. In the light of this, dayglow emissions of the Martian atmosphere are considered. It has been found that the red and green lines of OI and a number of spectral features of CO should be present and that their emission heights should be about 110-210 km from the surface of Mars.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.01(4) [December 1972]en_US
dc.titleCO Emission in the Martian Dayglowen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.01(4) [December 1972]

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