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dc.date.accessioned2023-03-04T16:07:32Z
dc.date.available2023-03-04T16:07:32Z
dc.date.created2022-05-13T13:39:38Z
dc.date.issued2022
dc.identifier.citationKotova, Daria Jin, Yaqi Miloch, Wojciech Jacek . Interhemispheric variability of the electron density and derived parameters by the Swarm satellites during different solar activity. Journal of Space Weather and Space Climate. 2022, 12, 1-21
dc.identifier.urihttp://hdl.handle.net/10852/100826
dc.description.abstractWith the data from the Swarm satellite mission, we study the variability of ionospheric plasma parameters for low and high solar activities. We focus on the electron density measured by Swarm and derived parameters and analyze the variability of these parameters in the contexts of the Northern and Southern hemispheres, specific latitudinal regions, and the solar activity level. We consider two time intervals: with high solar activity (HSA) from August 2014 to July 2015 and with low solar activity (LSA) from January to December 2018. We show that the electron density is described mainly by three probability density functions (PDF): exponentiated Weibull, lognormal, and chi distributions. These results with PDFs can be applied to the modeling or prediction of ionospheric parameters in different regions. The best fit of PDFs was obtained for low and mid-latitudes, while at high latitudes and in the polar caps, the double-peaked features of the distribution require the fit of multiple PDFs. The electron density (Ne) distribution at low latitudes follows more a lognormal distribution, while in the high latitude region, the chi distribution prevails. Different results were obtained for the rate of change of density index (RODI) with two fitting PDFs: lognormal or exponentiated Weibull, where the best fits are for high latitudes and polar caps. We demonstrate high variability in the electron density and derived parameters at low latitudes and in the polar caps. Comparing both hemispheres, we obtained higher values of these parameters during the solar minimum in the Southern hemisphere at high latitudes and polar caps, while for the Northern hemisphere, higher values were obtained at low latitudes. The dependence on the satellite’s altitude was also considered. The main patterns in the diurnal variation of parameters in different regions do not depend on the level of solar activity (which affects only the maximum values). The largest asymmetry between both hemispheres in Ne diurnal distribution was obtained for the polar cap regions. Here a 50% decrease in Ne was observed in the Northern hemisphere during HSA in the early morning sector (04–07 Magnetic Local Time), which has not yet been observed in the Southern hemisphere. For the first time, such a global statistical characterization of the ionospheric plasma density based on the in situ data is presented.
dc.languageEN
dc.publisherEDP Sciences
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleInterhemispheric variability of the electron density and derived parameters by the Swarm satellites during different solar activity
dc.title.alternativeENEngelskEnglishInterhemispheric variability of the electron density and derived parameters by the Swarm satellites during different solar activity
dc.typeJournal article
dc.creator.authorKotova, Daria
dc.creator.authorJin, Yaqi
dc.creator.authorMiloch, Wojciech Jacek
cristin.unitcode185,15,4,0
cristin.unitnameFysisk institutt
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin2024393
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Space Weather and Space Climate&rft.volume=12&rft.spage=1&rft.date=2022
dc.identifier.jtitleJournal of Space Weather and Space Climate
dc.identifier.volume12
dc.identifier.doihttps://doi.org/10.1051/swsc/2022007
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn2115-7251
dc.type.versionPublishedVersion
cristin.articleid12
dc.relation.projectNFR/267408
dc.relation.projectNFR/275655
dc.relation.projectEC/H2020/866357


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