CMS-Flow:Hydro Eqs: Difference between revisions

From CIRPwiki
Jump to navigation Jump to search
Deleted (talk | contribs)
Deleted (talk | contribs)
Line 7: Line 7:
- eps_{ij3} f_c u_j h = g \frac{\partial \eta }{\partial x_j}
- eps_{ij3} f_c u_j h = g \frac{\partial \eta }{\partial x_j}
  + \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[ \mu  h \frac{\partial C_{sa} }{\partial x_j} \biggr ]
  + \frac{\tau_i }{\rho}
  + \frac{\tau_i }{\rho}
</math>
</math>


<math>
  + \frac{\partial }{\partial x_j} \biggl[ \mu  h \frac{\partial C_{sa} }{\partial x_j} \biggr ] </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 22:04, 12 May 2010

Governing Equation

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

        ht+(huj)xj=S
        (hui)t+(huiuj)xjepsij3fcujh=gηxj+1ρ0paxj+xj[μhCsaxj]+τiρ


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.