Annotation
An integral numerical model is discussed which allows one to determine the density of the heat flux from water to air under the conditions of free convection in a nonaerated water mass. The primary external model parameters include the water and air temperatures and the air humidity and do not include the temperature of the underlying water surface. The calculated heat losses from a basin are compared with experimental data.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
Ya.L. Aleksandrov, E.P. Anisimova, S.N. Dikarev, A.A. Speranskaya, O.A. Speranskaya
Department of Marine and Inland Water Physics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Department of Marine and Inland Water Physics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
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