2010
DOI: 10.1016/j.asr.2010.02.030
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Regional VTEC modeling with multivariate adaptive regression splines

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Cited by 29 publications
(21 citation statements)
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“…Alongside the parametric approaches, other methods are also presented for VTEC modeling, such as neuralnetworks (Hernández-Pajares et al 1997), kriging (Wielgosz et al 2003) and multivariate adaptive regression splines (MARS) (Durmaz et al 2010). Later, Durmaz and Karslioglu (2011) introduced a multivariate adaptive regression B-splines (BMARS) algorithm for VTEC modeling, which is derived from MARS with a scale-by-scale model building strategy using compactly supported B-splines (Bakin and Hegland 1997;Bakin et al 2000a, b).…”
Section: Introductionmentioning
confidence: 99%
“…Alongside the parametric approaches, other methods are also presented for VTEC modeling, such as neuralnetworks (Hernández-Pajares et al 1997), kriging (Wielgosz et al 2003) and multivariate adaptive regression splines (MARS) (Durmaz et al 2010). Later, Durmaz and Karslioglu (2011) introduced a multivariate adaptive regression B-splines (BMARS) algorithm for VTEC modeling, which is derived from MARS with a scale-by-scale model building strategy using compactly supported B-splines (Bakin and Hegland 1997;Bakin et al 2000a, b).…”
Section: Introductionmentioning
confidence: 99%
“…Several research groups have provided GNSS-based solutions regarding the TEC modeling with appropriate approaches for quality assessment; for example, see Rovira-Garcia et al (2015), Li et al (2015), Brunini et al (2011) and Orus et al (2007). In the context of quality assessment, through a GPS phase-continuous arc, differential STEC, i.e., dSTEC values, can be obtained with an accuracy of less than 0.1 TECU (Feltens et al, 2011). Note that 1 TECU is equivalent to 10 16 electrons m −2 .…”
Section: Self-consistency Analysismentioning
confidence: 99%
“…A common approach, generally denoted as single-layer model (SLM), is based on the assumption that the electrons in the ionosphere are concentrated within a thin shell at a fixed altitude above the Earth (Mannucci et al, 1998;Komjathy and Langley, 1996). The spatial variations of electron content in this single layer are represented by a proper mathematical model such as spherical harmonics (Schaer, 1999), B-splines (Schmidt, 2007;Schmidt et al, 2008), spatially defined total electron content (TEC) grids (Skone, 1999), polynomials (Komjathy and Langley, 1996;Komjathy, 1997), wavelets (Schmidt, 2007), or the MARS (Durmaz et al, 2010) and BMARS approaches (Durmaz and Karslioglu, 2015). Furthermore, three-dimensional models that consider the variation with altitude were also studied (Hernández-Pajares et al, 1999;Mitchell and Spencer, 2003;Liu, 2004;Zeilhofer et al, 2009;Limberger et al, 2013).…”
Section: E Erdogan Et Al: Near Real-time Estimation Of Ionosphere Vtecmentioning
confidence: 99%
“…MARS is an adaptive method requiring no gridding of the input space. Durmaz et al (2010) applied MARS to regional VTEC modeling over a large part of Europe successfully. Subsequently Multivariate Adaptive Regression B-Splines (BMARS) was presented by Durmaz and Karslioglu (2011) with tensor product B-splines as basis functions obtained from observation locations.…”
Section: Introductionmentioning
confidence: 99%