Titlebook: Ionospheric Modeling; Jurij N. Korenkov Book 1988 Springer Basel AG 1988 atmospheric sciences.modeling

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Numerical Modeling of the High-Latitude F-Layer Anomalies,three-dimensional distribution of electron density, electron and ion temperature. The effects of auroral particle precipitation on the density and temperature structures are studied for winter and low solar activity conditions. The high-latitude ionospheric features, such as ‘the tongue of ionizatio

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Modeling of the Planetary Structure of the Ionosphere and the Protonosphere Coupling,ontinuity and motion for the ions O. and H. is presented. Some numerical results of model calculations are compared with the experimental data. The important role of electromagnetic drifts in the formation of large-scale morphological peculiarities of the ionosphere and the protonosphere coupling is

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Modelling of the Lower Ionosphere,ns. The effective rate coefficients were received from detailed models of ionization-recombination cycle. The calculations, which were made, and the comparisons with experimental data (Ne-profiles and their variations, absorption of radiowaves) have showed, that in general the model described the ba

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An Investigation of the Dependence of Structural Parameters of the Middle Atmosphere on the Intensindence of atmospheric structural parameters on temperature, solar activity, and on turbulent transfer intensity. For mesospheric heights, an inverse dependence of the nitric oxide density on the temperature has been found. It is thus possible to explain experimentally obtained temperature variations

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Electron Loss and the Determination of Electron Concentrations in the ,-Region,g of this region, would appear to be through use of the effective electron recombination coefficient, ? = ./[.]., where . is the ionization production rate, and where [.] is the electron concentration. This ratio apparently increases monotonically with decreasing altitude, and is much less variable

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,Modelling of Neutral-Gas Releases into the Earth’s Ionosphere,here. A study is made of neutral-gas expansion processes as well as of processes associated with the formation of decreased plasma density regions, ionospheric ‘holes’. The spatial-temporal distribution of particles released during the transition to the diffusion regime is constructed using an appro

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The Nighttime Winter Anomaly (NWA) Effect in the American Sector as a Consequence of Interhemispher and vertical sounding measurements in Havana (Cuba). An effective interhemispheric transport of plasma is suggested to explain enhanced northern nighttime ionization during winter solstice. To elucidate this effect, an adequate physical-numerical model of the coupled system ionosphere-plasmasphere

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Minimal Joule Dissipation Models of Magnetospheric Convection,nal slab model of the ionosphere featuring an enhanced conductivity auroral oval is used to compute high-latitude electric fields and currents. Mathematical methods used in the modeling include Fourier analysis, fast Fourier transforms, and variational calculus. Also, conformai transformations are i

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The Role of Vibrationally Excited Nitrogen in the Ionosphere,ar-resonant system in the . and . regions is taken into account. We describe our understanding of the methods necessary to find the vibrational populations of N. and CO. (asymmetric mode of CO.). The calculations of the vibrational temperatures in the ., ., and . regions for the mid-latitude ionosph