Ozone decline and its effect on night airglow intensity of Na 5893 Å at Dumdum (22.5°N, 88.5°E) and Halley Bay (76°S, 27°W)
The paper presents the effect of O^sub 3^ depletion on night airglow emission of Na 5893 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 Na 5893 Å line will also be a...
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| Veröffentlicht in: | Journal of Earth System Science 2006-10, Vol.115 (5), p.607-613 |
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| creator | Jana, P. K. Nandi, S. C. |
| description | The paper presents the effect of O^sub 3^ depletion on night airglow emission of Na 5893 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 Na 5893 Å line will also be affected due to the depletion of O^sub 3^ concentration. The nature of yearly variation and seasonal variation of the intensity of Na 5893 Å line for the above two stations are shown and compared. It is shown that the rate of decrease of intensity of Na 5893 Å line is comparatively more at Halley Bay due to the dramatic decrease of Antarctic O^sub 3^ concentration. A possible explanation for this dramatic decrease of Antarctic O^sub 3^ concentration is also mentioned.[PUBLICATION ABSTRACT] |
| doi_str_mv | 10.1007/BF02702913 |
| format | Article |
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K. ; Nandi, S. C.</creator><creatorcontrib>Jana, P. K. ; Nandi, S. C.</creatorcontrib><description>The paper presents the effect of O^sub 3^ depletion on night airglow emission of Na 5893 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 Na 5893 Å line will also be affected due to the depletion of O^sub 3^ concentration. The nature of yearly variation and seasonal variation of the intensity of Na 5893 Å line for the above two stations are shown and compared. It is shown that the rate of decrease of intensity of Na 5893 Å line is comparatively more at Halley Bay due to the dramatic decrease of Antarctic O^sub 3^ concentration. A possible explanation for this dramatic decrease of Antarctic O^sub 3^ concentration is also mentioned.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 0253-4126</identifier><identifier>EISSN: 0973-774X</identifier><identifier>DOI: 10.1007/BF02702913</identifier><language>eng</language><publisher>Bangalore: Springer Nature B.V</publisher><subject>Airglow ; Chemical kinetics ; Depletion ; Emissions ; Kinetics ; Nightglow ; Ozone ; Reaction kinetics ; Seasonal variation ; Seasonal variations ; Service stations</subject><ispartof>Journal of Earth System Science, 2006-10, Vol.115 (5), p.607-613</ispartof><rights>Indian Academy of Sciences 2006</rights><rights>Printed in India 2006.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2373-545a508819dd026302763134fb21a7995d971b6e08e2e7eabf8eca03bb8157d23</citedby><cites>FETCH-LOGICAL-c2373-545a508819dd026302763134fb21a7995d971b6e08e2e7eabf8eca03bb8157d23</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Jana, P. 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A possible explanation for this dramatic decrease of Antarctic O^sub 3^ concentration is also mentioned.[PUBLICATION ABSTRACT]</description><subject>Airglow</subject><subject>Chemical kinetics</subject><subject>Depletion</subject><subject>Emissions</subject><subject>Kinetics</subject><subject>Nightglow</subject><subject>Ozone</subject><subject>Reaction kinetics</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Service stations</subject><issn>0253-4126</issn><issn>0973-774X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1Uc1OwkAY3BhNRPTiE3zRixiK-9Pt7h4FQUwIHNTordm2WywpLfYnpp68-D48A76Yi5h48jRzmMxkZhA6JbhHMBZX_RGmAlNF2B5qYSWYI4T7vG855cxxCfUO0VFZLjBmnhSqhT5m73lmIDJhmljUWQRJVYKJYxNWkGeQJfOXCnRSzNP8DZKsMlmZVA3kMUw1cKkYfH2CruCmXkb1Ei4o7fHNetoFKbdk2PkxHes0NQ30dQMXwtus77tAxWb91DlGB7FOS3Pyi230OBo-DMbOZHZ7N7ieOCFltgZ3ueZYSqKiCFOP2ZoeI8yNA0q0UIpHSpDAM1gaaoTRQSxNqDELAkm4iChro_Od76rIX2tTVv4ir4vMRvp2LsVsiJ2rjc7-VRGXEEqYsqLLnSgs8rIsTOyvimSpi8Yn2N_e4P_dwL4BC6x2Zg</recordid><startdate>20061001</startdate><enddate>20061001</enddate><creator>Jana, P. 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| fulltext | fulltext |
| identifier | ISSN: 0253-4126 |
| ispartof | Journal of Earth System Science, 2006-10, Vol.115 (5), p.607-613 |
| issn | 0253-4126 0973-774X |
| language | eng |
| recordid | cdi_proquest_journals_2919337397 |
| source | Indian Academy of Sciences; EZB-FREE-00999 freely available EZB journals; SpringerLink Journals - AutoHoldings |
| subjects | Airglow Chemical kinetics Depletion Emissions Kinetics Nightglow Ozone Reaction kinetics Seasonal variation Seasonal variations Service stations |
| title | Ozone decline and its effect on night airglow intensity of Na 5893 Å at Dumdum (22.5°N, 88.5°E) and Halley Bay (76°S, 27°W) |
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