Using Principal Component Analysis of Satellite and Ground Magnetic Data to Model the Equatorial Electrojet and Derive Its Tidal Composition

dc.bibliographicCitation.firstPagee2022JA030691
dc.bibliographicCitation.issue9
dc.bibliographicCitation.journalTitleJGR : Space Physicseng
dc.bibliographicCitation.volume127
dc.contributor.authorSoares, Gabriel
dc.contributor.authorYamazaki, Yosuke
dc.contributor.authorMorschhauser, Achim
dc.contributor.authorMatzka, Jürgen
dc.contributor.authorPinheiro, Katia J.
dc.contributor.authorStolle, Claudia
dc.contributor.authorAlken, Patrick
dc.contributor.authorYoshikawa, Akimasa
dc.contributor.authorHozumi, Kornyanat
dc.contributor.authorKulkarni, Atul
dc.contributor.authorSupnithi, Pornchai
dc.date.accessioned2023-01-30T06:09:52Z
dc.date.available2023-01-30T06:09:52Z
dc.date.issued2022
dc.description.abstractThe intensity of the equatorial electrojet (EEJ) shows temporal and spatial variability that is not yet fully understood nor accurately modeled. Atmospheric solar tides are among the main drivers of this variability but determining different tidal components and their respective time series is challenging. It requires good temporal and spatial coverage with observations, which, previously could only be achieved by accumulating data over many years. Here, we propose a new technique for modeling the EEJ based on principal component analysis (PCA) of a hybrid ground-satellite geomagnetic data set. The proposed PCA-based model (PCEEJ) represents the observed EEJ better than the climatological EEJM-2 model, especially when there is good local time separation among the satellites involved. The amplitudes of various solar tidal modes are determined from PCEEJ based tidal equation fitting. This allows to evaluate interannual and intraannual changes of solar tidal signatures in the EEJ. On average, the obtained time series of migrating and nonmigrating tides agree with the average climatology available from earlier work. A comparison of tidal signatures in the EEJ with tides derived from neutral atmosphere temperature observations show a remarkable correlation for nonmigrating tides such as DE3, DE2, DE4, and SW4. The results indicate that it is possible to obtain a meaningful EEJ spectrum related to solar tides for a relatively short time interval of 70 days.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11150
dc.identifier.urihttp://dx.doi.org/10.34657/10176
dc.language.isoeng
dc.publisherHoboken, NJ : Wiley
dc.relation.doihttps://doi.org/10.1029/2022ja030691
dc.relation.essn2169-9402
dc.relation.issn2169-9380
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subject.ddc550
dc.subject.ddc520
dc.subject.otheratmospheric tideseng
dc.subject.otherequatorial electrojeteng
dc.subject.othergeomagnetismeng
dc.titleUsing Principal Component Analysis of Satellite and Ground Magnetic Data to Model the Equatorial Electrojet and Derive Its Tidal Compositioneng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccess
wgl.contributorIAP
wgl.subjectGeowissenschaftenger
wgl.subjectPhysikger
wgl.typeZeitschriftenartikelger
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