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		<doi>10.1002/2017JA024009</doi>
		<issn>2169-9402</issn>
		<citationkey>VenkateshRamFagSeeBat:2017:PaDa17</citationkey>
		<title>Electrodynamic disturbances in the Brazilian equatorialand low-latitude ionosphere on St. Patrick’s Daystorm of 17 March 2015</title>
		<year>2017</year>
		<month>Apr.</month>
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		<author>Venkatesh, K.,</author>
		<author>Ram, S. Tulasi,</author>
		<author>Fagundes, P. R.,</author>
		<author>Seemala, Gopi K.,</author>
		<author>Batista, Inez Staciarini,</author>
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		<group>DIDAE-CGCEA-INPE-MCTIC-GOV-BR</group>
		<affiliation>Universidade do Vale do Paraíba (UNIVAP)</affiliation>
		<affiliation>Indian Institute of Geomagnetism</affiliation>
		<affiliation>Universidade do Vale do Paraíba (UNIVAP)</affiliation>
		<affiliation>Indian Institute of Geomagnetism</affiliation>
		<affiliation>Instituto Nacional de Pesquisas Espaciais (INPE)</affiliation>
		<electronicmailaddress>venkatkau@gmail.com</electronicmailaddress>
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		<electronicmailaddress>inez.batista@inpe.br</electronicmailaddress>
		<journal>Journal of Geophysical Research: Space Physics</journal>
		<volume>122</volume>
		<number>4</number>
		<pages>4553-4570</pages>
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		<keywords>equatorial ionization anomaly, prompt penetration electric field, St. Patrick's day storm, super fountain effect.</keywords>
		<abstract>The St. Patrick's Day storm of 17 March 2015 has a long-lasting main phase with the Dst reaching a minimum of &#8722;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 F2 layer peak (hmF2) experienced a rapid uplift without any significant change in the base height (h&#8242;F); while the F2 layer is redistributed into F2 and F3 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.</abstract>
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		<language>en</language>
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