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- W37663048 abstract "The surface heat balance is applied to a lake's surface. The net heat flux through the surface determines the temperature response of the water. Assuming advective conditions and the formation of an inversion above the lake the water temperature is got as a result. Only the meteorological data of the surroundings upwind the well-mixed lake and its depth are needed to get solutions. An equilibrium temperature with no heat flux through the surface is defined. Applied to daily cycles of the surface temperature of lakes in the arid zones of the trades generally one harmonic is sufficient to describe the water temperature. This was shown by comparison of computed values with surface temperature measurements taken from a satellite (NIMBUS 4)." @default.
- W37663048 created "2016-06-24" @default.
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- W37663048 date "1979-01-01" @default.
- W37663048 modified "2023-10-03" @default.
- W37663048 title "The Daily Cycle of the water Temperature of a Shallow Lake" @default.
- W37663048 cites W1965152858 @default.
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- W37663048 doi "https://doi.org/10.1016/s0167-5648(08)70404-0" @default.
- W37663048 hasPublicationYear "1979" @default.
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