CMS-Flow:Subgrid Turbulence Model: Difference between revisions

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In CMS-Flow eddy viscosity is calculated as  
In CMS-Flow eddy viscosity is calculated as  
      <math> \nu_{t} = \nu_{t0} + \nu_c  + \nu_w  </math>
where  <math>\nu_{t0}</math> is a base value approximately equal to the dynamic viscosity, and <math>c_0</math> is an empirical coefficient approximately equal to 1/6,  <math>c_{sm}</math> is an empirical coefficient (Smagorinsky coefficient) between 0.25-0.5, 
The wave component of the eddy viscosity is calculated as
      <math> \nu_w = k(D/\rho)^{1/3} </math>
where <math>k</math> is an empirical coefficient, <math> \rho </math> is the water density, and <math>D</math> is the total wave dissipation.


       <math> \nu_{tc} = \nu_{t0} + \sqrt{ (c_0 u_* h)^2 + (c_{sm}^2 \Delta x \Delta y |S| )^2 } + k(D/\rho)^{1/3}</math>
       <math> \nu_{tc} = \nu_{t0} + \sqrt{ (c_0 u_* h)^2 + (c_{sm}^2 \Delta x \Delta y |S| )^2 } + k(D/\rho)^{1/3}</math>
where  <math>\nu_{t0}</math> is a base value approximately equal to the dynamic viscosity, and <math>c_0</math>  is an empirical coefficient and  <math>c_{sm}</math>  is an empirical coefficient (Smagorinsky coefficient).


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'''References'''
LARSON, M.; HANSON, H., and KRAUS, N. C., 2003. Numerical modeling of beach topography change. Advances in Coastal Modeling, V.C. Lakhan (eds.), Elsevier Oceanography Series, 67, Amsterdam, The Netherlands, 337-365.


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[[CMS-Flow]]
[[CMS-Flow]]

Revision as of 23:13, 2 November 2009

Subgrid Turbulence Model

In CMS-Flow eddy viscosity is calculated as

     νt=νt0+νc+νw

where νt0 is a base value approximately equal to the dynamic viscosity, and c0 is an empirical coefficient approximately equal to 1/6, csm is an empirical coefficient (Smagorinsky coefficient) between 0.25-0.5,

The wave component of the eddy viscosity is calculated as

     νw=k(D/ρ)1/3

where k is an empirical coefficient, ρ is the water density, and D is the total wave dissipation.

     νtc=νt0+(c0u*h)2+(csm2ΔxΔy|S|)2+k(D/ρ)1/3


CMS-Flow