The Role of Storm Time Electrodynamics in Suppressing the Equatorial Plasma Bubble Development in the Recovery Phase of a Geomagnetic Storm

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dc.contributor.author Sripathi, S.
dc.contributor.author Banola, S.
dc.contributor.author Emperumal, K.
dc.contributor.author Kumar, B. Suneel
dc.contributor.author Radicella, Sandro M.
dc.date.accessioned 2011-06-17T23:31:48Z
dc.date.accessioned 2021-02-12T10:11:39Z
dc.date.available 2011-06-17T23:31:48Z
dc.date.available 2021-02-12T10:11:39Z
dc.date.issued 2018
dc.identifier.citation JGR, 123, 2336–2350, doi: 10.1002/2017JA024956 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/1210
dc.description.abstract We investigate the role of storm time electrodynamics in suppressing the equatorial plasma bubble (EPB) development using multi-instruments over India during a moderate geomagnetic storm that occurred on 2 October 2013 where Dst minimum reached ~ 80 nT. This storm produced unique signatures in the equatorial ionosphere such that equatorial electrojet strength showed signatures of an abrupt increase of its strength to 150 nT and occurrence of episodes of counter electrojet events. During the main phase of the storm, the interplanetary magnetic field Bz is well correlated with the variations in the equatorial electrojet/counter electrojet suggesting the role of undershielding/overshielding electric fields of magnetospheric origin. Further, observations showed the presence of strong F3 layers at multiple times at multiple stations due to undershielding electric field. Interestingly, we observed simultaneous presence of F3 layers and suppression of EPBs in the dusk sector during the recovery phase. While strong EPBs were observed before and after the day of the geomagnetic storm, suppression of the EPBs on the storm day during “spread F season” is intriguing. Our further analysis using low-latitude station, Hyderabad, during the time of prereversal enhancement suggests that intense Esb layers were observed on the storm day but were absent/weak on quiet days. Based on these results, we suggest that the altitude/latitude variation of disturbance dynamo electric fields/disturbance winds may be responsible for simultaneous detection of F3 layers, occurrence of low-latitude Es layers, and suppression of EPBs during the storm day along the sunset terminator. en_US
dc.language.iso en_US en_US
dc.subject Electrodynamics en_US
dc.subject Geomagnetic storm en_US
dc.subject Equatorial Plasma bubble en_US
dc.subject EPBs en_US
dc.title The Role of Storm Time Electrodynamics in Suppressing the Equatorial Plasma Bubble Development in the Recovery Phase of a Geomagnetic Storm en_US
dc.type Article en_US
dc.identifier.accession 091744


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