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dc.contributor.authorJana, P K-
dc.contributor.authorSarkar, D-
dc.contributor.authorDas, P-
dc.date.accessioned2008-11-19T06:28:57Z-
dc.date.available2008-11-19T06:28:57Z-
dc.date.issued2008-10-
dc.identifier.issn0367-8393-
dc.identifier.urihttp://hdl.handle.net/123456789/2459-
dc.description326-332en_US
dc.description.abstractThe paper presents the effect of O3 depletion on night airglow emission of Li 6708 Å line at Dumdum (22.5°N, 88.5°E), India and Halley Bay (76°S, 27°W), a British Antarctic Service Station. Calculations based on chemical kinetics show that the airglow intensity of Li 6708 Å line will also be affected due to the depletion of O3 concentration. The nature of yearly variation and seasonal variation of intensity of Li 6708 Å line for the above two stations are shown and compared. It is shown that the rate of decrease of intensity of Li 6708 Å line is comparatively more at Halley Bay due to dramatic decrease of Antarctic O3 concentration.en_US
dc.language.isoen_USen_US
dc.publisherCSIRen_US
dc.sourceIJRSP Vol.37(5) [October 2008]en_US
dc.subjectOzone depletionen_US
dc.subjectAirglow emissionen_US
dc.subjectHalley Bayen_US
dc.subjectDumdumen_US
dc.titleEffect of long-term ozone trend on night airglow intensity of Li 6708 Å at Dumdum (22.5°N, 88.5°E) and Halley Bay (76°S, 27°W)en_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.37(5) [October 2008]

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