Annotation
Estimations of heat flows from the ocean to the atmosphere in drop transport during storms are given. It is shown that: (1) heat transport by sprays generated by strong wind and wave collapse is insignificant, compared with turbulent transport; (2) sprays promote heat transport from the lower to the higher atmosphere.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
V.N. Aksenov, E.G. Andreev, I.N. Ivanova, M.R. Kuznetsova, I.N. Tkacheva, G.G. Khundzhua
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