Planetary Variations in the Height of the F2-Layer Maximum during Ionospheric Disturbances

Author:

Sergeenko N. P.,Depueva A. Kh.

Publisher

Pleiades Publishing Ltd

Subject

Space and Planetary Science,Geophysics

Reference14 articles.

1. Aksenov, O., Yu., Kozlov S.I., Lyakhov A.N., Trekin V.V., Perunov Yu.M., and Yakubovskii, S.V., Analyzing existing applied models of the ionosphere for calculating radio wave propagation and possibility of their use for radar systems. 1. Classification of applied models and the main requirements imposed on them for radar aids, J. Sol.-Terr. Phys., 2020, vol. 6, no. 1, pp. 69–76.

2. Alpatov, V.V., Bekker, S.Z., Kozlov, S.I., Lyakhov, A.N., Yakim, V.V., and Yakubovskii, S.V., Analyzing existing applied models of the ionosphere to calculate radio wave propagation and a possibility of their use for radar-tracking systems. 2. Domestic models, J. Sol.-Terr. Phys., 2020, vol. 6, no. 3, pp. 60–66.

3. Altadill, D., Magdaleno, S., Torta, J.M., and Blanch, E., Global empirical models of the density peak height and of the equivalent scale height for quiet conditions, Adv. Space Res., 2012, vol. 52, pp. 1756–1769. https://doi.org/10.1016/j.asr.2012.11.018

4. Bilitza, D. and Eyfrig, R., A global model for the height of the F2-peak using M3000 values from the CCIR numerical map, Telecommun. J., 1979, vol. 46, no. 9, pp. 549–553.

5. Bryunelli, B.E. and Namgaladze, A.A., Fizika ionosfery (Ionospheric Physics), Moscow: Nauka, 1988.

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