Variation of the Equatorial Height Anomaly During the Main Phase of 2015 St. Patrick's Day Geomagnetic Storm Using ANNIM and TIEGCM

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dc.contributor.author Gowtam, V. Sai
dc.contributor.author Lei, Jiuhou
dc.contributor.author Tulasiram, S.
dc.contributor.author Luan
dc.date.accessioned 2010-11-13T16:39:33Z
dc.date.accessioned 2021-02-12T10:21:47Z
dc.date.available 2010-11-13T16:39:33Z
dc.date.available 2021-02-12T10:21:47Z
dc.date.issued 2019
dc.identifier.citation JGR, 124, doi: 10.1029/ 2019JA026703 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/1671
dc.description.abstract A double‐peak structure in the peak height of ionospheric F2 layer around ±10o geomagnetic latitudes similar to the equatorial ionization anomaly was recently reported. This unique feature was referred as the equatorial height anomaly (EHA). In the present paper, a simulation study is carried out using the data‐driven artificial neural network‐based two‐dimensional ionospheric model (ANNIM‐2D) and the physics‐based thermosphere‐ionosphere‐electrodynamics general circulation model (TIEGCM) to understand the local time and latitudinal variation of EHA during the main phase of St. Patrick's Day geomagnetic storm. Both the ANNIM‐2D and TIEGCM consistently show pronounced EHA during the main phase of the geomagnetic storm. Further, the local time of EHA development on the storm day is much earlier (nearly 2 hr) than the quiet time over Brazilian sector (90°W). The TIEGCM simulation revealed that the storm time enhancement of the equatorial fountain associated with the enhanced equatorial zonal electric field is the main controlling factor for the pronounced EHA during the main phase. The storm time meridional neutral winds positively contribute to the development of EHA. This study revealed the direct manifestation of the storm time‐enhanced plasma fountain on the EHA. en_US
dc.language.iso en_US en_US
dc.subject Geomagnetic storm en_US
dc.subject ANNIM en_US
dc.subject St. Patrick's Day en_US
dc.subject TIEGCM en_US
dc.title Variation of the Equatorial Height Anomaly During the Main Phase of 2015 St. Patrick's Day Geomagnetic Storm Using ANNIM and TIEGCM en_US
dc.type Article en_US
dc.identifier.accession 091844


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