Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.13091/2953
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dc.contributor.authorBaşçiftçi, F.-
dc.contributor.authorBülbül, Sercan-
dc.date.accessioned2022-10-08T20:49:59Z-
dc.date.available2022-10-08T20:49:59Z-
dc.date.issued2022-
dc.identifier.issn2785-339X-
dc.identifier.issn2785-2970-
dc.identifier.urihttps://doi.org/10.4430/bgo00394-
dc.identifier.urihttps://hdl.handle.net/20.500.13091/2953-
dc.description.abstractIt is important to be able to predict the occurrence time of an earthquake in order to take measures against its destructive effects. One of the parameters to be considered in earthquake prediction is ionospheric changes. Numerous studies have shown some changes in the ionosphere layer before or after the earthquake. These changes can be modelled to be detected with different methods and devices. One of the main parameters in examining these methods is the change of the Total Electron Content (TEC). With Global Navigation Satellite Systems (GNSS) observations, the TEC changes in the ionosphere can be determined before, during and after the earthquake. In this study, the changes in the ionosphere caused by the Seferihisar-Izmir earthquake (37.8881?? N 26.7770?? E, 30 October 2020, MW 6.6) were investigated in a 58-day time interval, including pre-earthquake, earthquake day, and post-earthquake. Firstly, the indices of solar activity (F10.7), Geomagnetic Activity (Dst), and Geomagnetic Storm (Kp) that can affect the ionosphere change pre-earthquake, earthquake day, and post-earthquake were examined. Then, the effects of the earthquake on the TEC changes in the ionosphere were investigated with the TEC values obtained from the regional ionospheric TEC (RIM-TEC), obtained from GNSS receivers in the earthquake zone and its surroundings, and global TEC maps (CODE). The indices showed that there were no geomagnetic activities between 29 September and 25 November 2020. In the study carried out, it was concluded that it is more accurate to calculate TEC values regionally rather than from Global TEC maps in the case of major episodic effects such as earthquakes. In addition, in the results about the TEC anomaly, it would seem that there was a maximum anomaly 8 days before the 304th day of 2020.en_US
dc.language.isoenen_US
dc.publisherIst Nazionale Di Oceanografia E Di Geofisicaen_US
dc.relation.ispartofBulletin of Geophysics and Oceanographyen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectGNSSen_US
dc.subjectionosphereen_US
dc.subjectSeferihisar-Izmir earthquakeen_US
dc.subjectspace weather conditionsen_US
dc.subjectTECen_US
dc.subjectTotal Electron-Contenten_US
dc.subjectGps-Tecen_US
dc.subjectAnomaliesen_US
dc.subjectRegionen_US
dc.subjectTurkeyen_US
dc.subjectDelayen_US
dc.subjectMapen_US
dc.titleInvestigation of ionospheric TEC changes potentially related to Seferihisar-Izmir earthquake (30 October 2020, M-W 6.6)en_US
dc.typeArticleen_US
dc.identifier.doi10.4430/bgo00394-
dc.identifier.scopus2-s2.0-85138231912en_US
dc.departmentFakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Harita Mühendisliği Bölümüen_US
dc.authorwosidBULBUL, Sercan/ABF-6270-2021-
dc.identifier.volume63en_US
dc.identifier.issue3en_US
dc.identifier.startpage403en_US
dc.identifier.endpage426en_US
dc.identifier.wosWOS:000834248000001en_US
dc.institutionauthorBülbül, Sercan-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.authorscopusid36545782700-
dc.authorscopusid57196346482-
dc.identifier.scopusqualityQ3-
item.cerifentitytypePublications-
item.grantfulltextembargo_20300101-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.openairetypeArticle-
item.fulltextWith Fulltext-
crisitem.author.dept02.08. Department of Geomatic Engineering-
Appears in Collections:Mühendislik ve Doğa Bilimleri Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collections
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collections
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