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Mechanisms of stratification of the F2 layer and formation of the F3 and G layers in the equatorial ionosphere

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Abstract

The paper is dedicated to the studies of formation mechanisms of additional layers in the equatorial ionosphere carried out using numerical simulations with use of the Global Self-Consistent Model of the Thermosphere, Ionosphere, and Protonosphere (GSM TIP) modified in the part of the solution of the electric field equation in the Earth’s ionosphere. Calculations were preformed for quiet geomagnetic conditions using the MSIS-90 model for the calculation of thermospheric parameters. The obtained spatio-temporal pattern of thermospheric circulation and the variations in the dynamo electric field obtained on its basis make it possible to reproduce the stratification effect of the F2 layer and the appearance of the F3 layer in the equatorial ionosphere due to the action of the nonuniform in height zonal electric field at the geomagnetic equator. On the basis of the earlier presented results of calculations using the modified GSM TIP model, the appearance of a maximum in the vertical profile of the electron density at a height of ∼1000 km formed by H+ ions, which we called the G layer, has been predicted. Numerical simulations showed that this layer is formed by the meridional component of the thermospheric wind and is related to the formation of the nighttime midlatitude maximum at heights of the ionospheric F region.

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Authors and Affiliations

  1. Institute of Terrestrial Magnetism, Ionosphere, and Radiowave Propagation, West Department, Russian Academy of Sciences, Kaliningrad, Russia

    M. V. Klimenko & V. V. Klimenko

  2. Kaliningrad State Technical University, Kaliningrad, Russia

    M. V. Klimenko

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  1. M. V. Klimenko
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  2. V. V. Klimenko
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Correspondence to M. V. Klimenko.

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Original Russian Text © M.V. Klimenko, V.V. Klimenko, 2012, published in Geomagnetizm i Aeronomiya, 2012, Vol. 52, No. 3, pp. 342–355.

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Klimenko, M.V., Klimenko, V.V. Mechanisms of stratification of the F2 layer and formation of the F3 and G layers in the equatorial ionosphere. Geomagn. Aeron. 52, 321–334 (2012). https://doi.org/10.1134/S0016793212030097

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