A response of the mid-latitude ionosphere to propagation of the atmospheric gravity wave

E. L. Afraimovich; A. F. Yakovets; V. V. Vodyannikov; G. I. Cordienko; Ya. F. Ashkaliev; Yu. G. Litvinov; S. B. Akasov

doi:10.1117/12.783392

14 February 2008 A response of the mid-latitude ionosphere to propagation of the atmospheric gravity wave

E. L. Afraimovich, A. F. Yakovets, V. V. Vodyannikov, G. I. Cordienko, Ya. F. Ashkaliev, Yu. G. Litvinov, S. B. Akasov

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Proceedings Volume 6936, Fourteenth International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics; 69361A (2008) https://doi.org/10.1117/12.783392
Event: Fourteenth International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics, 2007, Buryatia, Russian Federation

Abstract

This study reports observations of the response of the mid-latitude ionospheric F-layer to the passage of the atmospheric gravity wave (AGW) produced by the July 2004 geomagnetic storm, using data from the ground ionosonde located at Alma-Ata (43.25°N, 76.92°E). Ionograms were recorded every 5 min. They were analysed for temporal variations of virtual heights of specific frequencies (the virtual heights of a constant electron density), critical frequencies of the F-layer (f_o,xF) and height profiles of the electron density (N(h)-profiles). The temporal behaviour of all F-layer parameters such as the altitude of its peak (h_mF), the electron density at the peak (NmF) and the half thickness of the layer (ΔhF) revealed well-defined wave structures throughout the entire night of 24-25 July 2004. A comprehensive understanding of the relationship between phases of various parameters of the F-layer is established. It is shown that the relationship between phases of h_mF, NmF and ΔhF variations is determined by the value of the wave front tilt. As a rule, the certain phase of ΔhF precedes that of h_mF, and NmF anticorrelates with ΔhF. Last result contrast with previous investigations, which have frequently assumed a negative correlation between NmF and h_mF. A small amplitude of NmF variations compared with N(t) at certain altitudes may be largely explained in terms of the height gradient of AGW amplitudes.

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E. L. Afraimovich, A. F. Yakovets, V. V. Vodyannikov, G. I. Cordienko, Ya. F. Ashkaliev, Yu. G. Litvinov, and S. B. Akasov "A response of the mid-latitude ionosphere to propagation of the atmospheric gravity wave", Proc. SPIE 6936, Fourteenth International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics, 69361A (14 February 2008); https://doi.org/10.1117/12.783392

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KEYWORDS

Atmospheric propagation

Wave propagation

Magnetism

Particles

Atmospheric physics

Atmospheric plasma

Wavefronts

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