CMS-Flow:Hydro Eqs: Difference between revisions

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== Governing Equation ==
== Governing Equation ==
The depth-averaged 2-D continuity and momentum equations are given by
The depth-averaged 2-D continuity and momentum equations are given by
        <math> \frac{\partial h  }{\partial t} + \frac{\partial (h U_j )}{\partial x_j} = S </math>


{{Equation|<math> \frac{\partial h  }{\partial t} + \frac{\partial (h U_j )}{\partial x_j} = S </math>|2=1}}
{{Equation|<math> \frac{\partial h  }{\partial t} + \frac{\partial (h U_j )}{\partial x_j} = S </math>|2=1}}
\begin{equation} \label{eq:solve}
x^2 - 5 x + 6 = 0
\end{equation}


for  <math>  j=1,2  </math>
for  <math>  j=1,2  </math>


        <math> \frac{\partial ( h U_i ) }{\partial t} + \frac{\partial (h U_i U_j )}{\partial x_j}
{{Equation| <math> \frac{\partial ( h U_i ) }{\partial t} + \frac{\partial (h U_i U_j )}{\partial x_j}
- \epsilon_{ij3} f_c U_j h = - g h \frac{\partial \eta }{\partial x_j}
- \epsilon_{ij3} f_c U_j h = - g h \frac{\partial \eta }{\partial x_j}
  - \frac{h}{\rho_0} \frac{\partial p_a }{\partial x_j}
  - \frac{h}{\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}
  + \frac{\tau_i }{\rho}
  </math>   
  </math>|2=2}}  


for <math> i=1,2 </math> and <math> j=1,2 </math>
for <math> i=1,2 </math> and <math> j=1,2 </math>

Revision as of 21:06, 18 May 2010

Governing Equation

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

  (1)

for

  (2)

for and

Symbol Description Units
Time sec
Total water depth m
Still water depth m
Water surface elevation with respect to the still water elevation m
Current velocity in the jth direction m/sec
Sum of Precipitation and evaporation per unit area m/sec
Gravitational constant m/sec2
Water density kg/m3
Atmospheric pressure Pa
Turbulent eddy viscosity m2/sec

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