We develop and apply non-local theoretical and numerical model to study the stability of Rayleigh–Taylor (RT) modes in the Earth's atmosphere in the presence of dusty plasma. We use fluid equations and the dynamics of charged dust grains to obtain an eigenmode equation to study the stability of the RT mode. Typical ionospheric parameters are used to investigate the stability of the mode. The growth rate of the RT is found to be considerably higher in a dusty plasma than in a pure plasma. This might be the clue in explaining the origin of low-frequency modes in the ionosphere. We also study the effects of the dust charge, the dust mass, the density scale length and the dust density on the growth rate of the instability.
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