The bottom shear stress is given by
| 1) |
\displaystyle \boldsymbol{\tau}_b = \rho C_D | \boldsymbol{V} | \boldsymbol{V} |
where
\rho: water density [M/L3]
C_D : non-dimensional drag coefficient [-]
The drag coefficient is computed using the Manning’s roughness coefficient as
| 2) |
\displaystyle C_D = \frac{n^2 g}{R^{1/3}} |
in which
n: Manning's roughness coefficient [T/L1/3]
R: hydraulic radius [L]
g: gravitational acceleration [L/T2]
Dividing by \rho R gives the friction term of the momentum equation,
|
\dfrac{ \boldsymbol{\tau}_b }{ \rho R } = c_b \left\| \boldsymbol{V} \right\| \boldsymbol{V} , \qquad c_b = \dfrac{ C_D }{ R } = \dfrac{ g n^2 }{ R^{4/3} } |
where c_b is the nonlinear friction coefficient [1/L].
For the semi-implicit treatment the term is collected as a linear-plus-quadratic drag acting on the velocity,
|
\dfrac{ \boldsymbol{\tau}_b }{ \rho R } = c_f \, \boldsymbol{V}, \qquad c_f = c_L + c_b \left\| \boldsymbol{V} \right\| |
where
c_f : total friction coefficient [1/T]
c_L : linear friction coefficient [1/T]
The linear coefficient is zero by default; it is available for cases where a linear damping is physically appropriate (e.g. very shallow laminar sheet flow) or where mild additional damping is desired. A constant nonlinear drag coefficient may also be specified in place of Manning's law for idealized studies. The quadratic part of the friction term reproduces the familiar Manning friction slope,
|
c_b \left\| \boldsymbol{V} \right\| \boldsymbol{V} = g \, \boldsymbol{S}_f , \qquad \boldsymbol{S}_f = \dfrac{ n^2 \left\| \boldsymbol{V} \right\| \boldsymbol{V} }{ R^{4/3} } |
where \boldsymbol{S}_f is the friction slope vector [-]
The scalar friction slope S_f specified for normal-depth boundary conditions (see Flow and Stage Boundary Conditions) is the magnitude of this vector.
The shear velocity is given by:
| 3) |
\displaystyle u_* = \sqrt{\tau_b / \rho } |