CMS-Flow:Hydro Eqs: Difference between revisions

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  + \frac{1}{\rho_0} \frac{\partial p_a }{\partial x_j}
  + \frac{1}{\rho_0} \frac{\partial p_a }{\partial x_j}
+ \frac{\partial }{\partial x_j} \biggl[ \nu_t  h \frac{\partial u_i }{\partial x_j} \biggr ]
+ \frac{\partial }{\partial x_j} \biggl[ \nu_t  h \frac{\partial u_i }{\partial x_j} \biggr ]
  + \frac{\tau_i }{\rho}   <nowiki>for </nowiki> i=1,2 <nowiki>and </nowiki> j=1,2 </math>
  + \frac{\tau_i }{\rho}
</math>   for <math> i=1,2 </math> and <math> j=1,2 </math>


where <math> t </math> is time, <math> u_j </math> is the current velocity in the jth direction, <math> h </math> is the total water depth, <math>  C_{sa} </math> is the salinity concentration, and <math> K_{sa} </math> is the salinity mixing coefficient.
where <math> t </math> is time, <math> u_j </math> is the current velocity in the jth direction, <math> h </math> is the total water depth, <math>  C_{sa} </math> is the salinity concentration, and <math> K_{sa} </math> is the salinity mixing coefficient.

Revision as of 22:12, 12 May 2010

Governing Equation

The depth-averaged 2-D continuity and momentum equations are given by

        ht+(huj)xj=Sforj=1,2
        (hui)t+(huiuj)xjϵij3fcujh=gηxj+1ρ0paxj+xj[νthuixj]+τiρ   for i=1,2 and j=1,2

where t is time, uj is the current velocity in the jth direction, h is the total water depth, Csa is the salinity concentration, and Ksa is the salinity mixing coefficient.