Height dependence of the amplitude of ionospheric wave disturbances

Details Height dependence of the amplitude of ionospheric wave disturbances Height dependence of the amplitude of ionospheric wave disturbances

Aug 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986ge%26ae..26..680d&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 26, July-Aug. 1986, p. 680-682. In Russian.

Computer Science

Ionospheric Disturbances, Vertical Distribution, Wave Propagation, Amplitudes, Atmospheric Density, Height, Wave Attenuation

Scientific paper

The height dependence of background wave disturbances (WDs) was measured at Alma-Ata during January-February 1985. The height dependence of the relative WD amplitude is determined by two competing factors: (1) amplitude increase due to a decrease in atmospheric density with height and (2) WD dissipation, increasing with height. It is shown that the height dependence leads to the formation of an amplitude peak at a specific height; the peaks of the high-frequency WD components are shifted to lower heights as compared with low-frequency components.

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