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dc.contributor.authorGhodpage, R.N.
dc.contributor.authorSiingh, Devendraa
dc.contributor.authorSingh, R.P.
dc.contributor.authorMukherjee, G.K.
dc.contributor.authorVohat, P.
dc.contributor.authorSingh, A.K.
dc.date.accessioned2016-12-20T12:01:36Z
dc.date.accessioned2021-02-12T09:45:49Z-
dc.date.available2016-12-20T12:01:36Z
dc.date.available2021-02-12T09:45:49Z-
dc.date.issued2012
dc.identifier.citationJournal of Earth System Science, v.121/6, p.1511-1525, 2012, doi: 10.1007/s12040-012-0240-4en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/943-
dc.description.abstractSimultaneous photometric measurements of the OI 557.7 nm and OH (7, 2) band from a low latitude station, Kolhapur (16.8°N, 74.2°E) during the period 2004–2007 are analyzed to study the dominant waves present in the 80–100 km altitude region of the atmosphere. The nocturnal intensity variations of different airglow emissions are observed using scanning temperature controlled filter photometers. Waves having period lying between 2 and 12 hours have been recorded. Some of these waves having subharmonic tidal oscillation periods 4, 6, 8 and 12 hours propagate upward with velocity lying in the range 1.6–11.3 m/s and the vertical wave length lying between 28.6 and 163 kms. The other waves may be the upward propagating gravity waves or waves resulting from the interaction of inter-mode tidal oscillations, interaction of tidal waves with planetary waves and gravity waves. Some times, the second harmonic wave has higher vertical velocity than the corresponding fundamental wave. Application of these waves in studying the thermal structure of the region is discussed.en_US
dc.language.isoenen_US
dc.subjectTidal and gravity waveen_US
dc.subjectAirglow emissionen_US
dc.subjectMesosphere and lower thermosphere (MLT)en_US
dc.subjectPlanetary wavesen_US
dc.subjectKolhapuren_US
dc.titleTidal and gravity waves study from the airglow measurements at Kolhapur (India)en_US
dc.typeArticleen_US
dc.identifier.accession091266
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