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Theoretical modeling of convection II. Reynolds Stress Model
2006
Proceedings of the International Astronomical Union
The Reynolds Stress Model (RSM) yields the dynamic equations for the secondorder moments (e.g., heat fluxes) needed in the equations for the mean variables (e.g., mean temperature). The RSM equations are in general time dependent and non-local. We first discuss the "buoyancy only" case and the tests of the non-local model against a variety of data. We also "plumenize" the model in order to exhibit the up-down flows that characterize convection so as to show that a non-local RSM is fully
doi:10.1017/s1743921307000063
fatcat:v5m6yi47xbfd7bq7iuii46xc7a