CMS-Flow:Hydro Eqs: Difference between revisions

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         <math> \frac{\partial ( h u_i ) }{\partial t} + \frac{\partial (h u_i u_j )}{\partial x_j}
         <math> \frac{\partial ( h u_i ) }{\partial t} + \frac{\partial (h u_i u_j )}{\partial x_j}
- eps_{ij3} f_c u_j h = g \frac{\partial \eta }{\partial x_j}
- \epsilon_{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[ \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 ]

Revision as of 22:07, 12 May 2010

Governing Equation

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

        ht+(huj)xj=S
        (hui)t+(huiuj)xjϵij3fcujh=gηxj+1ρ0paxj+xj[νthuixj]+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.