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The discretized momentum equations are  
The discretized momentum equations are  
<math> \frac{\partial h}{\partial t} \int_{A_p} U_i
+ \oint_{F} \frac{\partial (h U_i U_j )}{\partial x_j}
- \epsilon_{ij3} f_c U_j h = - g h \frac{\partial \eta }{\partial x_i}
- \frac{h}{\rho_0} \frac{\partial p_a }{\partial x_i}
+ \frac{\partial }{\partial x_j} \biggl ( \nu_t  h \frac{\partial U_i }{\partial x_j} \biggr )
+ \frac{\tau_i }{\rho}
</math>


<math> U_{i,P}^{n+1} = \frac{1}{a_{i,P}} \biggl( \sum_{k=1} a_{i,k} U_{i,k}^{n+1} + S_i \biggr)  
<math> U_{i,P}^{n+1} = \frac{1}{a_{i,P}} \biggl( \sum_{k=1} a_{i,k} U_{i,k}^{n+1} + S_i \biggr)  
- \frac{h_P}{a_{i,P}} \sum_{k=1} n_{ik} \Delta s_k p_k^{n+1}
- \frac{h_P}{a_{i,P}} \sum_{k=1} n_{ik} \Delta s_k p_k^{n+1}
</math>
</math>
The continuity equation is discretized as
<math> h^{n+1} -  \mathbf{S} </math>


where the subscript <math>k</math> indicates the cell face, <math>p = g \eta</math> with <math>\eta</math> being the water surface elevation, <math>n_{ik}</math> is equal to the dot product of the velocity unit vector and the cell face unit vector.  
where the subscript <math>k</math> indicates the cell face, <math>p = g \eta</math> with <math>\eta</math> being the water surface elevation, <math>n_{ik}</math> is equal to the dot product of the velocity unit vector and the cell face unit vector.  
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The continuity equation is discretized as
The continuity equation is discretized as
<math> p_P^{n+1} = p_P^n - g \frac{\Delta t}{\Delta A_P} \sum_{k=1} n_k F_k^{n+1}</math>
where <math>n_k </math> is the dot product of the cell face unit vector and


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

Revision as of 23:54, 29 January 2011

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The discretized momentum equations are htApUi+F(hUiUj)xjϵij3fcUjh=ghηxihρ0paxi+xj(νthUixj)+τiρ


Ui,Pn+1=1ai,P(k=1ai,kUi,kn+1+Si)hPai,Pk=1nikΔskpkn+1

The continuity equation is discretized as

hn+1𝐒


where the subscript k indicates the cell face, p=gη with η being the water surface elevation, nik is equal to the dot product of the velocity unit vector and the cell face unit vector.

The coefficient ai,P is equal to ai,P=ai,k+aP0

The continuity equation is discretized as pPn+1=pPngΔtΔAPk=1nkFkn+1

where nk is the dot product of the cell face unit vector and


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

  ht+(hUj)xj=S (1)

for j=1,2

  (hUi)t+(hUiUj)xjϵij3fcUjh=ghηxihρ0paxi+xj(νthUixj)+τiρ (2)