CMS-Flow:Subgrid Turbulence Model: Difference between revisions

From CIRPwiki
Jump to navigation Jump to search
Line 3: Line 3:


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).


----
----
'''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.


----
----
</big>
</big>
[[CMS-Flow]]
[[CMS-Flow]]

Revision as of 23:13, 2 November 2009

Subgrid Turbulence Model

In CMS-Flow eddy viscosity is calculated as

     

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

The wave component of the eddy viscosity is calculated as

     

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

     


CMS-Flow