The Effect of the Midlatitude Electron Density Trough on the Ionospheric Conductivities

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dc.authoridÜNAL, İbrahim/0000-0001-8497-4459
dc.authoridTimocin, Erdinc/0000-0002-3648-2035
dc.authorwosidÜNAL, İbrahim/ABH-5657-2020
dc.authorwosidTimocin, Erdinc/H-2855-2017
dc.contributor.authorTimocin, Erdinc
dc.contributor.authorUnal, Ibrahim
dc.contributor.authorYesil, Ali
dc.date.accessioned2024-08-04T20:45:43Z
dc.date.available2024-08-04T20:45:43Z
dc.date.issued2019
dc.departmentİnönü Üniversitesien_US
dc.description.abstractIn this study, we have investigated the effect of midlatitude electron density trough on ionospheric conductivities for different altitudes. For this purpose, parallel conductivity (sigma (0)), Pedersen conductivity (sigma (1)) and Hall conductivity (sigma (2)) data were calculated by using the International Reference Ionosphere (IRI) model for seven different geographic coordinates in the midlatitude region of the northern hemisphere during the June and December solstices of 1972. Planetary geomagnetic activity index () data are used as a geomagnetic activity indicator. These conductivity values computed for each position were classified according to geomagnetic active () and geomagnetic quiet () conditions; and these values were examined according to invariant magnetic latitudes (I >) for different heights, seasonal, geomagnetic activity and local times. From the analysis results, it is found that the midlatitude electron density trough does not have any effects on sigma (0) for all situations, but the trough is influential on sigma (1) and sigma (2) during night hours of the December solstices. In addition, it was observed that the trough increased its effect on sigma (1) and sigma (2) with the increasing geomagnetic activity level and altitude for December solstices.en_US
dc.identifier.doi10.1007/s40995-018-0578-9
dc.identifier.endpage307en_US
dc.identifier.issn1028-6276
dc.identifier.issn2364-1819
dc.identifier.issueA1en_US
dc.identifier.scopus2-s2.0-85061753134en_US
dc.identifier.scopusqualityQ2en_US
dc.identifier.startpage297en_US
dc.identifier.urihttps://doi.org/10.1007/s40995-018-0578-9
dc.identifier.urihttps://hdl.handle.net/11616/98659
dc.identifier.volume43en_US
dc.identifier.wosWOS:000458550900033en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSpringer International Publishing Agen_US
dc.relation.ispartofIranian Journal of Science and Technology Transaction A-Scienceen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectIonosphereen_US
dc.subjectIonospheric conductivitiesen_US
dc.subjectMidlatitude electron density troughen_US
dc.subjectMagnetosphereen_US
dc.titleThe Effect of the Midlatitude Electron Density Trough on the Ionospheric Conductivitiesen_US
dc.typeArticleen_US

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