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Electrodynamic disturbances in the Brazilian equatorial and low‐latitude ionosphere on St. Patrick's Day storm of 17 March 2015
Author(s) -
Venkatesh K.,
Tulasi Ram S.,
Fagundes P. R.,
Seemala Gopi K.,
Batista I. S.
Publication year - 2017
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1002/2017ja024009
Subject(s) - ionosphere , geology , geomagnetic storm , electric field , ionosonde , f region , storm , geophysics , dynamo , substorm , anomaly (physics) , total electron content , atmospheric sciences , climatology , earth's magnetic field , magnetic field , physics , magnetosphere , electron , tec , electron density , oceanography , condensed matter physics , quantum mechanics
The St. Patrick's Day storm of 17 March 2015 has a long‐lasting main phase with the Dst reaching a minimum of −223 nT. During the main phase, two strong prompt penetration electric field (PPEF) phases took place; first with the southward turning of IMF Bz around ~1200 UT and the second with the onset of a substorm around ~1725 UT leading to strong equatorial zonal electric field enhancements. The consequent spatiotemporal disturbances in the ionospheric total electron content and the resultant modifications in the equatorial ionization anomaly (EIA) over the Brazilian longitudinal sector are investigated in detail. The simultaneous measurements from a large network of GPS receivers, ionosonde, and magnetometers over the Brazilian longitudinal sector are used for this study. In the presence of enhanced zonal electric field, the equatorial F 2 layer peak ( h m F 2 ) experienced a rapid uplift without any significant change in the base height ( h ′ F ); while the F 2 layer is redistributed into F 2 and F 3 layers. The enhanced zonal electric filed due to PPEF led to the strong super fountain effect under which the anomaly crest departed poleward to ~40°S latitude. In the presence of westward and equatorward wind surge over Brazil with the coexisting disturbance dynamo fields, strong hemispheric asymmetry is seen in the storm time response of EIA during both the PPEF phases.