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Breaking tides, planetary, and gravity waves can also induce changes to thermospheric and ionospheric composition through eddy mixing.
Flow visualization observations show clearly that large scale eddy mixing can be generated in regions between sharp edges.
Lindzen (1967) suggested that diurnal tides can break down in the MLT region, generate turbulence, enhance the eddy mixing, and change the chemical compositions in that region and in higher thermosphere.
In addition to the AMOC, Marshall and Zanna (2014) used a conceptual model to point out the importance of ocean eddy mixing in the Southern Ocean, with larger mixing leading to a faster (yet smaller) global heat uptake response.
Because diurnal tides can affect the eddy mixing and change the chemical compositions in the MLT region, DE3 tide can change the NO and O2 densities in E-region and affect the E-region molecular ion (and electron) density (see Ren et al. 2012b).
The thermo-chemistry is evolved by stand-alone linear eddy mixing (LEM) model simulations under both premixed and non-premixed conditions, where the unsteady interaction of turbulence with chemical kinetics is included as a part of the training database.
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Equations for predicting the dependence of the eddy viscosity and mixing length on the dimensionless radial position in the pipe were obtained.
Turbulent characteristics of the far wake of the first turbine acting as the inflow for the downwind turbine were characterized calculating the eddy viscosity and mixing length profiles from the obtained data.
In deriving the set of equations for the calculation of eddy viscosity and mixing length we assumed the non-Newtonian character of the turbulent two phase solid particles-gas flow.
The eddy scales and mixing behaviour of the flows are assessed using several different metrics, and their dependence on liquid and gas flow rates in the foam is assessed and compared.
The possible differences in thermal stratification or mixing physics in the scaled-down model and the prototype SFR are evaluated by quantifying eddy thermal diffusivity and mixing efficiency.
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