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pro vyhledávání: '"Yu. G. Taranukha"'
Autor:
L. M. Belokrinitskaya, G. M. Kruchenitskii, L. V. Kozak, A. A. Rozhilo, V. N. Ivchenko, P. N. Kozak, Yu. G. Taranukha, V. G. Kruchinenko
Publikováno v:
Atmospheric and Oceanic Optics. 24:261-270
The problem of aerosol formation in the Earth’s upper atmosphere is considered. Meteoroids with masses of 10−18–10−8 g are taken as a source of their origin. Based on the classical equations of deceleration and heating of small meteor bodies,