2011
DOI: 10.1109/tap.2011.2122237
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The HF Channel EM Parameters Estimation Under a Complex Environment Using the Modified IRI and IGRF Model

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Cited by 18 publications
(12 citation statements)
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“…During the sunlit hours, all ionosphere layers are available, but when ionization effect of Sun disappears at night, -layer becomes the predominant layer in spite of a decrease in peak electron density [4], [10]. Two main characteristic parameters of this layer are the maximum ionization height (km) and the critical frequency (MHz).…”
Section: Iri-plas Model and Model Parametersmentioning
confidence: 99%
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“…During the sunlit hours, all ionosphere layers are available, but when ionization effect of Sun disappears at night, -layer becomes the predominant layer in spite of a decrease in peak electron density [4], [10]. Two main characteristic parameters of this layer are the maximum ionization height (km) and the critical frequency (MHz).…”
Section: Iri-plas Model and Model Parametersmentioning
confidence: 99%
“…IRI-Plas model with input and output parameter sets. radio communications [1], [10]. IRI-Plas model estimates critical frequency and height values by analyzing its preset coefficient matrices.…”
Section: Iri-plas Model and Model Parametersmentioning
confidence: 99%
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“…Ionosphere is the layer of the atmosphere that lies between 60 and 1,000 km above Earth's surface and comprises three distinct layers, namely, the D layer, E layer, and F layer, which is normally divided into F 1 and F 2 layers (Sezen et al, 2013;Yao et al, 2013). The critical frequency of the F 2 layer (f o F 2 ) is an important characteristic parameter that is widely applied in civil and military fields, such as high-frequency communication (Angling et al, 2009;Yan et al, 2011), satellite communication (Scherliess & Fejer, 1999), navigation (Mitch et al, 2013), timing, radar tracking (Yao et al, 2013), detection, localization (Swamy et al, 2013), and spectrum management (Wang et al, 2013).…”
Section: Introductionmentioning
confidence: 99%
“…This model has evolved into a number of important editions, including IRI-78 (Rawer et al, 1981), IRI-85, IRI-1990(Bilitza, 1990, IRI-2000(Bilitza, 2001, IRI-2007(Bilitza & Reinisch, 2008, IRI-2012(Bilitza et al, 2014, and IRI-2016 (Bilitza et al, 2017). Moreover, the Asia-Oceania method and its modified version were proposed to describe the monthly median values of f o F 2 and M3000F2, which apply well to the Asia and Oceania region (Cao & Sun, 2009;Yan et al, 2011). Oyeyemi et al (2005Oyeyemi et al ( , 2007; Oyeyemi and McKinnell (2008) and Bai et al (2018) used a neural network and extreme learning machine to develop new models of F 2 layer parameters.…”
Section: Introductionmentioning
confidence: 99%