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

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,Quasilinear Heating of Electrons in the Earth’s Plasmasphere,of the earth. For this type of ‘wave-particle’ interaction, a simplification of the quasilinear diffusion integral in a magneto-active plasma under plasmaspheric conditions is given. Under the assumption of a Maxwellian distribution of electrons we have calculated the collision frequency and the hea
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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 basic features of D-region parameters.
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2504-3625 Overview: 978-3-0348-6534-0978-3-0348-6532-6Series ISSN 2504-3625 Series E-ISSN 2504-3633
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Pageoph Topical Volumeshttp://image.papertrans.cn/i/image/475240.jpg
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Simulations of the Seasonal and Universal Time Variations of the High-Latitude Thermosphere and Ionng winter, the diurnal migration of the polar convection pattern into and out of sunlight, together with ion transport, plays a major role in the plasma density structure at F-region altitudes. Only during those UT periods, when the entire geomagnetic polar region is in total darkness, is the effect
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Global Model of the Thermosphere-Ionosphere-Protonosphere System,unt computed thermosphere and ionosphere parameters..The inputs needed for our global model are the solar EUV spectrum; the auroral precipitation pattern; the distribution of the field-aligned currents and the model of the geomagnetic field..Preliminary results are obtained without regard to electro
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