CMS-Flow:Hydro Eqs: Difference between revisions

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{{Equation| <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_i}
  - \frac{h}{\rho_0} \frac{\partial p_a }{\partial x_j}
  - \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{\partial }{\partial x_j} \biggl ( \nu_t  h \frac{\partial U_i }{\partial x_j} \biggr )
  + \frac{\tau_i }{\rho}
  + \frac{\tau_i }{\rho}

Revision as of 22:49, 12 August 2010

Governing Equation

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)

for i=1,2 and j=1,2

Symbol Description Units
t Time sec
h Total water depth h=ζ+η m
ζ Still water depth m
η Water surface elevation with respect to the still water elevation m
Uj Current velocity in the jth direction m/sec
S Sum of Precipitation and evaporation per unit area m/sec
g Gravitational constant m/sec2
ρ Water density kg/m3
pa Atmospheric pressure Pa
νt Turbulent eddy viscosity m2/sec

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