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• W1860637537 abstract "We present both fully resolved direct numerical simulation and large eddy simulation results for turbulent stratified flow in an open channel with periodic boundaries in the stream-wise direction and no-slip vertical sidewalls in the span-wise direction. A uniform heat source term is applied in the top 20% of the domain, approximating the solar heat flux into a river system. After each time step the total scalar flux input into the domain is uniformly removed allowing a fully developed flow field to be evolved and statistics collected. This approach allows fully developed stratified flow to be simulated with a density profile which includes a lower non-stratified region, steep thermocline and an upper laminar mixed layer region. The Reynolds number for the flows is in the range 5400-7300 and the bulk Richardson number in the range 0-0.4. References R. P. Garg, J. H. Ferziger, S. G. Monismith, and J. R. Koseff. Stably stratified turbulent channel flows. I. Stratification regimes and turbulence suppression mechanism. Phys. Fluids , 12(10):2569--2594, 2000. doi:10.1063/1.1288608 . S. Komori, H. Ueda, F. Ogino, and T. Mizushina. Turbulence structure in stably stratified open-channel flow. J. Fluid Mech. , 130:13--26, 1983. doi:10.1017/S0022112083000944 . Lei Wang and Xi-Yun Lu. Large eddy simulation of stably stratified turbulent open channel flows with low- to high-Prandtl number. Int. J. Heat and Mass Transfer , 48(10):1883 -- 1897, 2005. doi:10.1016/j.ijheatmasstransfer.2004.12.017 . J. R. Taylor, S. Sarkar, and V. Armenio. Large eddy simulation of stably stratified open channel flow. Phys. Fluids , 17(11):116602, 2005. doi:10.1063/1.2130747 . J. S. Turner. A note on wind mixing at the seasonal thermocline. Deep-Sea Res. , 16(Suppl.):297--300, 1969. P. E. Holloway. A criterion for thermal stratification in a wind-mixed System. J. Phys. Oceanogr. , 10:861--869, 1980. 2.0.CO;2>doi:10.1175/1520-0485(1980)010 2.0.CO;2 J. H. Simpson and J. R. Hunter. Fronts in the Irish sea. Nature , 250:404--406, 1974. doi:10.1038/250404a0 . M. Bormans and I. T. Webster. A mixing criterion for turbid rivers. Environmental Modelling and Software with Environment Data News , 12(4):329--333, 1997. doi:10.1016/S1364-8152(97)00032-7 . M. Germano, U. Piomelli, P. Moin, and W. H. Cabot. A dynamic subgrid-scale stress model. Phys. Fluids A , 3(7):1760--1765, 1991. doi:10.1063/1.857955 . S. B. Pope. Turbulent Flows . Cambridge University Press, 2000. S. W. Armfield and R. Street. Fractional step methods for the Navier--Stokes equations on non-staggered grids. ANZIAM Journal , 42:C134--C156, 2000. http://journal.austms.org.au/ojs/index.php/ANZIAMJ/article/view/593 . S. W. Armfield, S. E. Norris, P. Morgan, and R. Street. A parallel non-staggered Navier--Stokes solver implemented on a workstation cluster. In S. Armfield, P. Morgan, and K. Srinvas, editors, Proceedings of the Second International Conference on Computational Fluid Dynamics , pages 30--45, Sydney, July 15-19 2002. J. H. Ferziger and M. Peric. Computational Methods for Fluid Dynamics . Springer, third edition, 2002." @default.
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• W1860637537 date "2013-05-13" @default.
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• W1860637537 title "A canonical model for stratified flow in estuaries and rivers" @default.
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• W1860637537 doi "https://doi.org/10.21914/anziamj.v54i0.6429" @default.
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