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

被引:12
|
作者
Sripathi, S. [1 ,2 ]
Banola, S. [1 ]
Emperumal, K. [3 ]
Kumar, B. Suneel [4 ]
Radicella, Sandro M. [5 ]
机构
[1] Indian Inst Geomagnetism, New Bombay, India
[2] Abdus Salaam Int Ctr Theoret Phys, Trieste, Italy
[3] Indian Inst Geomagnetism, Equatorial Geophys Res Lab, Tirunelveli, India
[4] TIFR Balloon Launch Facil, Hyderabad, Andhra Pradesh, India
[5] Abdus Salaam Int Ctr Theoret Phys, Trieste, Italy
关键词
IONOSPHERIC ELECTRIC-FIELDS; SPORADIC-E; SCINTILLATION ACTIVITY; MAGNETIC STORM; LOW LATITUDES; SPREAD-F; E-REGION; ART; DISTURBANCES; PENETRATION;
D O I
10.1002/2017JA024956
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
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 similar to-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 F-3 layers at multiple times at multiple stations due to undershielding electric field. Interestingly, we observed simultaneous presence of F-3 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 E-sb 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 F-3 layers, occurrence of low-latitude E-s layers, and suppression of EPBs during the storm day along the sunset terminator.
引用
收藏
页码:2336 / 2350
页数:15
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