Abstract. The data analysis of the on-board instruments set of the Cosmos-1809 and IKB-1300 satellites is presented for the following events. Continuous sequence of tropical cyclones (TCs) after the Mounts Pinatubo and Hudson eruptions in 1991. Sequences of 3 super-typhoons in the Western Pacific in November 1990. Sequences of 5 hurricanes in the Atlantic Ocean in September 1981. It is shown that the effects of the several interacting TCs impact on the ionosphere differ from those of single TCs. The distribution of electron fluctuations and density, VLF-ELF oscillations, and other plasma parameters of the upper ionosphere varies at different stages of development of tropical disturbances. Models of TCs interaction that change the parameters of the ionosphere are proposed. An important role is played by acoustic oscillations generated in TCs. The strongest volcanic eruptions in the twentieth century threw a significant amount of aerosols into the stratosphere. It is discussed how stratosphere changes for interacting TCs and perturbations after volcanic eruptions apparently cause a redistribution of infrasound along the TCs track which can lead to the formation of new TCs.
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