An empirical model for the global distributions of density, temperature and effective collision frequency of electrons in the ionosphere

An improved ionospheric global empirical reference model (named RIM-85) is established for the distributions of density (N e), temperature (T e) and effective collision frequency ( ν e) of electrons between 65 and 600 km. For altitudes above 200 km, at low and middle latitudes, the N e distribution...

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Veröffentlicht in:Advances in space research 1987, Vol.7 (6), p.49-52
Hauptverfasser: Chasovitin, Yu.K., Shirochkov, A.V., Besprozvannaya, A.S., Gulyaeva, T.L., Denisenko, P.F., Armenskaya, O.A., Ivanova, S.E., Kashirin, A.I., Klyueva, N.M., Koryakina, E.A., Mironova, L.S., Sykilinda, T.N., Shushkova, V.B., Vodolazkin, V.I., Sotsky, V.V., Sheidakov, N.E.
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container_end_page 52
container_issue 6
container_start_page 49
container_title Advances in space research
container_volume 7
creator Chasovitin, Yu.K.
Shirochkov, A.V.
Besprozvannaya, A.S.
Gulyaeva, T.L.
Denisenko, P.F.
Armenskaya, O.A.
Ivanova, S.E.
Kashirin, A.I.
Klyueva, N.M.
Koryakina, E.A.
Mironova, L.S.
Sykilinda, T.N.
Shushkova, V.B.
Vodolazkin, V.I.
Sotsky, V.V.
Sheidakov, N.E.
description An improved ionospheric global empirical reference model (named RIM-85) is established for the distributions of density (N e), temperature (T e) and effective collision frequency ( ν e) of electrons between 65 and 600 km. For altitudes above 200 km, at low and middle latitudes, the N e distribution is based on IRI-82, with some necessary corrections. In comparison with IRI-82 and other models the model RIM-85 has a number of important advantages: (i) it describes in detail the height distributions of N e and T e below 200 km; (ii) it gives for the first time an adequate description of the high latitude ionosphere, its variations with geomagnetic activity reflecting the occurrence and dynamics of the main large-scale structures of the spatial N e distributions; (iii) it describes rather correctly the shape of the N e height profiles at low and high latitudes, in the outer ionosphere and also at high solar activity; (iv) it gives a spatial maximum height distribution of the F-region in the southern hemisphere which is close to the real one and (v) it describes rather correctly the diurnal and seasonal variations of T e. The model RIM-85 is established as a computer program, the general structure of which is similar to the corresponding programs for the IRI-79 and IRI-82 models; it includes some subroutines taken from this model software. Therefore the newly developed model can easily be included into a new version of IRI as a subprogram for N e, T es and ν e calculations.
doi_str_mv 10.1016/0273-1177(87)90270-5
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For altitudes above 200 km, at low and middle latitudes, the N e distribution is based on IRI-82, with some necessary corrections. In comparison with IRI-82 and other models the model RIM-85 has a number of important advantages: (i) it describes in detail the height distributions of N e and T e below 200 km; (ii) it gives for the first time an adequate description of the high latitude ionosphere, its variations with geomagnetic activity reflecting the occurrence and dynamics of the main large-scale structures of the spatial N e distributions; (iii) it describes rather correctly the shape of the N e height profiles at low and high latitudes, in the outer ionosphere and also at high solar activity; (iv) it gives a spatial maximum height distribution of the F-region in the southern hemisphere which is close to the real one and (v) it describes rather correctly the diurnal and seasonal variations of T e. 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For altitudes above 200 km, at low and middle latitudes, the N e distribution is based on IRI-82, with some necessary corrections. In comparison with IRI-82 and other models the model RIM-85 has a number of important advantages: (i) it describes in detail the height distributions of N e and T e below 200 km; (ii) it gives for the first time an adequate description of the high latitude ionosphere, its variations with geomagnetic activity reflecting the occurrence and dynamics of the main large-scale structures of the spatial N e distributions; (iii) it describes rather correctly the shape of the N e height profiles at low and high latitudes, in the outer ionosphere and also at high solar activity; (iv) it gives a spatial maximum height distribution of the F-region in the southern hemisphere which is close to the real one and (v) it describes rather correctly the diurnal and seasonal variations of T e. The model RIM-85 is established as a computer program, the general structure of which is similar to the corresponding programs for the IRI-79 and IRI-82 models; it includes some subroutines taken from this model software. Therefore the newly developed model can easily be included into a new version of IRI as a subprogram for N e, T es and ν e calculations.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/0273-1177(87)90270-5</doi><tpages>4</tpages></addata></record>
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subjects Earth, ocean, space
Exact sciences and technology
External geophysics
Ionospheric structure (d, e, f and topside regions)
Physics of the ionosphere
title An empirical model for the global distributions of density, temperature and effective collision frequency of electrons in the ionosphere
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