Evidence for the Influence of DE3 Tide on the Occurrence of Equatorial Counterelectrojet

dc.contributor.authorSingh, Dupinder
dc.contributor.authorGurubaran, S.
dc.contributor.authorHe, Maosheng
dc.date.accessioned2011-06-18T00:04:46Z
dc.date.accessioned2021-02-12T10:12:10Z
dc.date.available2011-06-18T00:04:46Z
dc.date.available2021-02-12T10:12:10Z
dc.date.issued2018
dc.description.abstractThe long-term Challenging Minisatellite Payload magnetometer data are analyzed to derive the equatorial counterelectrojet (CEJ) signatures globally over a range of local times. The resultant local time-longitude map of CEJ occurrence rate shows a strong influence of the diurnal eastward propagating wave number 3 (DE3) nonmigrating tide during July–September months. DE3 is also shown to account for the reduction of CEJ occurrence at certain longitudes. These aspects of DE3 tide-CEJ relationship have implications for understanding the seasonal and longitudinal variations of CEJ. Observations of zonal winds from the Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED) Doppler Interferometer instrument on board the TIMED satellite are used to establish these findings.en_US
dc.identifier.accession091745
dc.identifier.citationGeophysical Research Letters, 45, 2145–2150, doi: 10.1002/2018GL077076en_US
dc.identifier.urihttp://library.iigm.res.in:4000/handle/123456789/1211
dc.language.isoen_USen_US
dc.subjectAtmospheric tidesen_US
dc.subjectEquatorial Counterelectrojeten_US
dc.subjectCounterelectrojeten_US
dc.subjectCEJen_US
dc.titleEvidence for the Influence of DE3 Tide on the Occurrence of Equatorial Counterelectrojeten_US
dc.typeArticleen_US

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