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dc.contributor.authorPant, T.K.
dc.contributor.authorTiwari, D.
dc.contributor.authorVineeth, C.
dc.contributor.authorThampi, Smitha V.
dc.contributor.authorSridharan, S.
dc.contributor.authorDevasia, C.V.
dc.contributor.authorSridharan, R.
dc.contributor.authorGurubaran, S.
dc.contributor.authorSekar, R.
dc.date.accessioned2015-09-10T09:10:54Z
dc.date.accessioned2021-02-12T09:28:43Z-
dc.date.available2015-09-10T09:10:54Z
dc.date.available2021-02-12T09:28:43Z-
dc.date.issued2007
dc.identifier.citationGeophysical Research Letters, v34/15, L15102, 2007, doi: 10.1029/2007GL030193en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/374-
dc.description.abstract[1] This paper investigates the simultaneous presence of a prominent planetary scale modulations of quasi 16-day period observed in the daytime mean mesopause temperature and in the phase velocity of Type I electrojet irregularities during January–March 2001 over Trivandrum (8.5°N, 76.5°E, 0.5°N diplat.). The temperature was estimated from the Multiwavelength Dayglow Photometer (MWDPM) measurements of OH (8–3) Meinel band dayglow emissions. The radar measured phase velocity of the irregularities is found not only exhibiting ∼8 and quasi 16-day modulations, but also exceeding the isothermal ion-acoustic threshold i.e. ∼360 m/s for Trivandrum. The modulation in the mesopause temperature is attributed to the presence of planetary wave of quasi 16-day periodicity. Further, it is proposed that the temperature modulations which cause composition changes in the mesopause and equatorial electrojet region manifest as changes in the phase velocity through fluctuations in ion-neutral collisions corroborating with St.-Maurice et al. (2003).en_US
dc.language.isoenen_US
dc.subjectRadar measurementsen_US
dc.subjectEquatorial electrojeten_US
dc.subjectMesopause energeticsen_US
dc.subjectElectrojet irregularitiesen_US
dc.subjectEEJ irregularitiesen_US
dc.subjectMLTIen_US
dc.titleInvestigation on the mesopause energetics and its possible implications on the equatorial MLTI processes through coordinated daytime airglow and radar measurementsen_US
dc.typeArticleen_US
dc.identifier.accession090867
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