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HEAT BALANCE COMPONENTS OF LAKES AND RIVERS
SUMMER HEATING AND FALL COOLING
THE WINTER TEMPERATURE REGIME
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absorption of radiant advection air temperature albedo approximation assume atmosphere averaged water temperature bottom soil boundary conditions coefficient of heat coefficient of turbulent continuous ice cover course of water crystallization process depth determined diurnal course dynamic effective radiation enthalpy expression fall cooling Figure flow rate flux of radiant Fourier numbers Fourier series frazil freezing lakes function Gidrometizdat heat and moisture heat balance equation heat flux heat transfer ice crystals ice period initial data initial temperature distribution intensity of turbulent investigations Izvestiya AN SSSR Kolesnikov lakes and rivers Leningrad marine surface layer observation data obtained parameter problem quantitative radiant energy flux radiant energy penetrating slush ice snow cover solar radiation solution specific humidity storage lakes sun elevation supercooling temperature field temperature fluctuations temperature wave thermal conditions thermocline Trudy turbulent exchange coefficient turbulent heat exchange turbulent mixing underside variation vertically averaged water volume absorption water bodies water surface yields