Annotation
It is shown that the difference between the chemical composition of sea aerosols and that of sea water may be due to irreversible processes of heat and mass exchange between the ocean and the atmosphere. These processes may cause changes in the chemical composition of the ocean surface microlayer, which generates aerosols.
Rissian citation:
М.Р. Кузнецова, Е.В. Караваева, В.А. Твердислов.
Зависимость коэффициента фракционирования ионов в морских аэрозолях от интенсивности испарения с поверхности моря. Вестн. Моск. ун-та. Сер. 3. Физ. Астрон. 1992. № 5. С. 85.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
M.R. Kuznetsova, E.V. Karavaeva, V.A. Tverdislov
Department of Physics of Atmosphere and Mathematical Geophysics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Department of Physics of Atmosphere and Mathematical Geophysics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
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