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

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dc.contributor.author Singh, Dupinder
dc.contributor.author Gurubaran, S.
dc.contributor.author He, Maosheng
dc.date.accessioned 2011-06-18T00:04:46Z
dc.date.accessioned 2021-02-12T10:12:10Z
dc.date.available 2011-06-18T00:04:46Z
dc.date.available 2021-02-12T10:12:10Z
dc.date.issued 2018
dc.identifier.citation Geophysical Research Letters, 45, 2145–2150, doi: 10.1002/2018GL077076 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/1211
dc.description.abstract The 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.language.iso en_US en_US
dc.subject Atmospheric tides en_US
dc.subject Equatorial Counterelectrojet en_US
dc.subject Counterelectrojet en_US
dc.subject CEJ en_US
dc.title Evidence for the Influence of DE3 Tide on the Occurrence of Equatorial Counterelectrojet en_US
dc.type Article en_US
dc.identifier.accession 091745


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