“…Analysis and numerical calculations have shown that whistler waves decay more efficiently in the daytime ionosphere. This is due to the fact that the daytime lower boundary of the ionosphere is less sharp than the nighttime one, and whistler waves can penetrate into the region of strong absorption, where For the case of oblique incidence, the results of calculating the reflection coefficient were given in (Bespalov et al, 2018;Mizonova and Bespalov, 2021), on the basis of which, at reasonable amplitudes of the infrasonic wave, the depth of modulation of the logarithm of the reflection coefficient R r + ( )…”