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Estimation of frequency and duration of ionospheric disturbances over Turkey with IONOLAB-FFT algorithm

dc.contributor.authorKaratay S.
dc.contributor.authorKaratay, S
dc.date.accessioned2023-05-09T15:34:26Z
dc.date.available2023-05-09T15:34:26Z
dc.date.issued2020-09-01
dc.date.issued2020.01.01
dc.description.abstractOne of the more common methods of observation of variability of the Earth’s ionosphere is based on total electron content (TEC) estimated from ground-based dual-frequency Global Positioning System (GPS) receivers. Variations in solar, geomagnetic and seismic activity cause depletions or enhancements in the ionospheric electron concentrations that can be detected as disturbances. Some of these disturbances have wave-like characteristics, where frequency of oscillation can be used to identify and classify the disturbance. In this study, the frequency of such periodic disturbances is estimated using a fast Fourier transform (FFT)-based method, namely IONOLAB-FFT, in the spectral domain. IONOLAB-FFT, which was initially developed to be used on slant TEC (STEC), is modified to be applied to TEC in the local zenith direction of the receiver. The algorithm is tested using literature data on disturbances generated by a geomagnetic activity, a solar flare, a medium-scale traveling ionospheric disturbance (MSTID), a large-scale TID (LSTID) and an earthquake. An accordance with these known disturbances is observed in running IONOLAB-FFT, and the main frequencies and durations of the disturbances are estimated. IONOLAB-FFT method is applied to TEC computed from Turkish Permanent GPS Network (TNPGN-Active) which lies in mid-latitude region to detect the any wave-like oscillations, sudden disturbances and other irregularities during December, March, June and September months for 2010, 2011 and 2012 years. It is observed that a large number of the estimated frequencies are accumulated between 0.08 and 0.14 MHz corresponding to periods of 3.5 h to 2 h. The significant frequencies are grouped less than 0.28 MHz. A large number of the durations of the oscillations are between 425 and 550 min in 2010, 300 and 550 min in 2011 and 350 and 400 min in 2012. The longest duration (around 800 min: 13.33 h) is observed in December months, and the shortest duration (around 2 h) is observed in September months.
dc.identifier.doi10.1007/s00190-020-01416-1
dc.identifier.eissn1432-1394
dc.identifier.issn0949-7714
dc.identifier.scopus2-s2.0-85090017015
dc.identifier.urihttps://hdl.handle.net/20.500.12597/12410
dc.identifier.volume94
dc.identifier.wosWOS:000567891300001
dc.relation.ispartofJournal of Geodesy
dc.relation.ispartofJOURNAL OF GEODESY
dc.rightsfalse
dc.subjectDisturbances | FFT | GPS | Ionosphere | Total electron content
dc.titleEstimation of frequency and duration of ionospheric disturbances over Turkey with IONOLAB-FFT algorithm
dc.titleEstimation of frequency and duration of ionospheric disturbances over Turkey with IONOLAB-FFT algorithm
dc.typeArticle
dspace.entity.typePublication
oaire.citation.issue9
oaire.citation.volume94
relation.isScopusOfPublication2a0684d3-b529-49a1-9827-14fe119ec443
relation.isScopusOfPublication.latestForDiscovery2a0684d3-b529-49a1-9827-14fe119ec443
relation.isWosOfPublicationf3186e0b-0cf7-43ae-a5f4-49413c15d8cd
relation.isWosOfPublication.latestForDiscoveryf3186e0b-0cf7-43ae-a5f4-49413c15d8cd

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