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dc.contributor.authorGowtam, V. Sai
dc.contributor.authorLei, Jiuhou
dc.contributor.authorTulasiram, S.
dc.contributor.authorLuan
dc.date.accessioned2010-11-13T16:39:33Z
dc.date.accessioned2021-02-12T10:21:47Z-
dc.date.available2010-11-13T16:39:33Z
dc.date.available2021-02-12T10:21:47Z-
dc.date.issued2019
dc.identifier.citationJGR, 124, doi: 10.1029/ 2019JA026703en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/1671-
dc.description.abstractA 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.isoen_USen_US
dc.subjectGeomagnetic stormen_US
dc.subjectANNIMen_US
dc.subjectSt. Patrick's Dayen_US
dc.subjectTIEGCMen_US
dc.titleVariation of the Equatorial Height Anomaly During the Main Phase of 2015 St. Patrick's Day Geomagnetic Storm Using ANNIM and TIEGCMen_US
dc.typeArticleen_US
dc.identifier.accession091844
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