This paper presents a CFD modelling study of the bubble driven hydrodynamics in aluminium reduction cells. A time-averaged (steady state) bubble driven flow model has been developed using a full scale air-water model of part of an aluminium reduction cell as a test-bed. Simulated results have been compared with experimental data taken under similar conditions using Particle Image Velocimetry (P...

We present a one-equation subgrid scale model that evolves the turbulence energy corresponding to unresolved velocity fluctuations in large eddy simulations. The model is derived in the context of the Germano consistent decomposition of the hydrodynamical equations. The eddy-viscosity closure for the rate of energy transfer from resolved toward subgrid scales is localised by means of a dynamica...

7 The mechanisms of the atmospheric response to climate forcing are analyzed using an ex8 ample of uniform SST warming in an idealized aqua-planet model. A 200-member ensemble 9 of experiments is conducted with an instantaneous uniform SST warming. The zonal mean 10 circulation changes display a rapid poleward shift in the midlatitude eddy-driven westerlies 11 and the edge of the Hadley cell ci...

Dissipation and flux-variance methods, derived from the turbulent kinetic energy and temperature variance budget equations in conjunction with Monin-Obukov similarity theory, were used to estimate surface fluxes of momentum and sensible heat. To examine the performance of these two methods, direct eddy correlation measurements were carried out above a nonuniform grass-covered forest clearing in...

The small-scale roughness properties of the seafloor are increasingly being recognized as critical parameters in determining important processes in physical oceanography. For instance, in situ observations (e.g., Polzin et al., 1997) find that mixing levels are greatly elevated in regions of rough topography. Gille et al. (2000) demonstrate that mesoscale eddy energy tends to be lower in areas ...

In this study, we investigate the problems of inhomogeneous turbulence. The main goal has been to find the connections between analytic turbulence theories, notably the formalism of the direct interaction approximation (DIA), and turbulence phenomenology. To simplify the results from an inhomogeneous DIA model, we have employed a diagonalization procedure and an assumption of weak inhomogeneity...

A physically plausible lower bound on the spatially varying geostrophic mesoscale eddy energy dissipation time-scale within ocean, related to geographical transfer rate out of mesoscales, is provided by means a simple and computational inexpensive inverse calculation. Data diagnosed from high resolution global configuration ocean simulation supplied parameterized model energy, which results as ...