Estimation of hmF2 and foF2 communication parameters of ionosphere F2-layer üsing GPS data and IRI-plas model

buir.contributor.authorArıkan, Orhan
buir.contributor.orcidArıkan, Orhan|0000-0002-3698-8888
dc.citation.epage5273en_US
dc.citation.issueNumber10en_US
dc.citation.spage5264en_US
dc.citation.volumeNumber61en_US
dc.contributor.authorSezen, U.en_US
dc.contributor.authorSahin, O.en_US
dc.contributor.authorArikan, F.en_US
dc.contributor.authorArıkan, Orhanen_US
dc.date.accessioned2015-07-28T12:03:37Z
dc.date.available2015-07-28T12:03:37Z
dc.date.issued2013-10en_US
dc.departmentDepartment of Electrical and Electronics Engineeringen_US
dc.description.abstractF2-layer is the most important and characteristic layer of the ionosphere in the propagation of high frequency (HF) waves due to the highest level of conductivity in the propagation path. In this study, the relation of Total Electron Content (TEC) with the maximum ionization height (hmF2) and the critical frequency (foF2) of F2 -layer are investigated within their defined parametric range using the IRI model extended towards the plasmasphere (IRI-Plas). These two parameters are optimized using daily observed GPS-TEC (IONOLAB-TEC) in an iterational loop through Non-Linear Least Squares (NLSQ) optimization while keeping the physical correlation between hmF2 and foF2 parameters. Optimization performance is examined for daily (24-hour) and hourly TEC optimizations separately. It is observed that hourly TEC optimization produces results with much smaller estimation errors. As a result of the hourly optimization, we obtain the hourly hmF2 and foF2 estimates as they are the optimization parameters. Obtained hmF2 and foF2 estimates are compared with the ionosonde estimates for various low, middle and high latitude locations for both quite and disturbed days of ionosphere. The results show that hmF2 and foF2 estimates obtained from IRI-Plas optimization (IRI-Plas-Opt) and ionosonde are very much in agreement with each other. These results also signify that IRI-Plas provides a reliable background model for ionosphere. With the proposed method, it is possible to build a virtual ionosonde via optimization of IRI-Plas model using the observed TEC values.en_US
dc.identifier.doi10.1109/TAP.2013.2275153en_US
dc.identifier.issn0018-926X
dc.identifier.urihttp://hdl.handle.net/11693/12877
dc.language.isoEnglishen_US
dc.publisherIEEEen_US
dc.relation.isversionofhttp://dx.doi.org/10.1109/TAP.2013.2275153en_US
dc.source.titleIEEE Transactions on Antennas and Propagationen_US
dc.subjectFof2en_US
dc.subjectGpsen_US
dc.subjectHmf2en_US
dc.subjectIonolaben_US
dc.subjectIri-plasen_US
dc.subjectTecen_US
dc.subjectVirtual Ionosondeen_US
dc.titleEstimation of hmF2 and foF2 communication parameters of ionosphere F2-layer üsing GPS data and IRI-plas modelen_US
dc.typeArticleen_US

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