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A family of ionospheric models for different uses
Institution:1. Institut für Meteorologie and Geophysik, Universität Graz, Graz, Austria;2. Abdus Salam ICTP, Aeron. And Radioprop. Lab., Trieste, Germany;1. Radiophysical Research Institute Nizhny Novgorod State University, Nizhny Novgorod 603950, Russia;2. Kazan Federal University, Kazan 420000, Russia;3. Southern Federal University, Rostov-on-Don 344006, Russia;4. Mari State University, Yoshkar-Ola 424000, Russia;5. SITCOM LLC, Yoshkar-Ola 424031, Russia;1. Research Institute of Physics, Southern Federal University, Rostov-on-Don, 344090, Russia;2. Fedorov Institute of Applied Geophysics, Moscow, 129128, Russia;1. Institute of Earthquake Forecasting, China Earthquake Administration, Beijing, China;2. School of Electronic Information, Wuhan University, Wuhan, Hubei, China;3. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Abstract:Empirical models of three dimensional electron density distributions in the ionosphere have been constructed for global as well as regional use. The models differ by their degree of complexity and calculation time and therefore have different uses. All are based on “ionogram parameter” (critical frequencies foE, foF1, foF2 and the F2 region transfer parameter M(3000)F2). The models allow the use of global or regional maps for foF2 and M(3000)F2 and use built-in formulations for foE and foF1. Update (instantaneous mapping / nowcasting) versions exist which take foF2 and M(3000)F2 or F2 region peak height and electron density as input. The ground to F2 layer peak part of the profile is identical for all three models and is based on an Epstein formulation. The “quick calculationr” model NeQuick uses a simple formulation for the topside F layer, which is essentially a semi-Epstein layer with a thickness parameter which increases linearly with height. The “ionospheric model” COSTprof is the model which was adopted by COST 251 in its regional “monthly median” form. Its topside F layer is based on O+-H+ diffusive equilibrium with built-in maps for three parameters, namely the oxygen scale height at the F2 peak, its height gradient and the O+-H+ transition height. The “ionosphere-plasmasphere” model NeUoG-plas uses a magnetic field aligned “plasmasphere” above COSTprof Typical uses of the models and comparison among them are discussed.
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