AbstractTo study the relationship between the excitation source of gravity wave in the troposphere and the response of ionosphere, a theoretic model of gravity wave propagation based on the complex dispersion relation of internal gravity wave and the conception of transfer function has been built in a dissipative atmosphere which includes viscosity and heat conductivity. In this paper the amplitude of transfer function is discussed in the frequency domain. Through analyzing a case of unit impulse, we obtain the temporal and spatial distribution of a certain physical quantity from earth's surface to 300 km altitude. The results reveal that the atmosphere behaves like a filter which offers the easy passage to some gravity waves whose periods are between 15 min and 30 min and the horizontal wave lengths are between 200 km and 450 km, that it is large in horizontal distance between the source and the response of ionosphere, that the viscosity and the conductivity coefficients of atmosphere have little effect in the low atmosphere, but they become more and more important with the increment of height, and that the frequency obtained by transfer function model is consistent with Row's theory in the low atmosphere, but inconsistent in the high atmosphere.
Read full abstract