Circular Basin: Difference between revisions

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=Problem=
=Problem=
Dupont (2001) presented an analytical solution for a closed circular domain on an f-plane, with radius <math> R </math>, a linear bottom friction. The governing equations are
Dupont (2001) presented an analytical solution for a closed circular domain on an f-plane, with radius <math> R </math>, a linear bottom friction. The governing equations are
 
   {{Equation| <math> -f_c h U + g h \frac{\partial \eta}{\partial x} = \tau_{bx}+ \tau_{Wx} </math>|2=1}}
   {{Equation| <math> g h \frac{\partial \eta}{\partial x} + \frac{\partial (U_j h  C_{tk})}{\partial x_j} = \frac{\partial }{\partial x_j} </math>|2=1}}
  {{Equation| <math> f_c h V + g h \frac{\partial \eta}{\partial x} = \tau_{by}+ \tau_{Wy} </math>|2=2}}
 
where <math> \tau_{bx} = \kappa h U,  </math>, and a spatially variable wind stress equal to <math> \tau_{Wx} = Wy/R</math>, <math> \tau_{Wy} = 0 </math>  
<math> \tau_{bx} = \kappa h U,  </math>, and a spatially variable wind stress equal to <math> \tau_{Wx} = Wy/R</math>, <math> \tau_{Wy} = 0</math>  
where <math> W</math> is the gradient of the wind forcing and <math> y</math>  is the vertical coordinate.
where <math> W</math> is the gradient of the wind forcing and <math> y</math>  is the vertical coordinate.



Revision as of 22:10, 19 May 2011

UNDER CONSTRUCTION

Problem

Dupont (2001) presented an analytical solution for a closed circular domain on an f-plane, with radius R, a linear bottom friction. The governing equations are

  fchU+ghηx=τbx+τWx (1)
  fchV+ghηx=τby+τWy (2)

where τbx=κhU,, and a spatially variable wind stress equal to τWx=Wy/R, τWy=0 where W is the gradient of the wind forcing and y is the vertical coordinate.

Solution

The water surface elevation solution is given by

  η={Wr2sin2θ4gHR,if fc=0WfcRgHκ[R28+r24(κfcsin2θ1)],if fc0 (1)

The current velocities are independent of the Coriolis parameter and are given by

  u=Wy2Rκ (2)
  v=Wx2Rκ (3)

Setup

Figure 1. Computational grid.

The model is run to steady state from zero current and water level initial conditions with W=104m2s2, κ=103s1 , and fc=0. Table 1 shows the general settings used for CMS-Flow. Figure 1 shows the computational grid with 5 levels of refinement from 2000 m to 125 m.


Table 1. General Settings for Wind-driven flow in a circular basin

Parameter Value
Time step 3600 s
Simulation Duration 72 hrs
Ramp Period 24 hrs
Initial Water Depth 10 m
Mixing Terms Off
Wall Friction Off
Linear Bottom Friction Coefficient 0.001



Results

Figure 1. Analytical current velocities and water levels.
Figure 1. Calculated current velocities and water levels.


Table 2. Goodness of fit statistics for the current velocity and water level

Variable RRMSE, % RMAE, % R^2 Bias
U-Velocity 3.88 0.64 0.997 -4.06e-5
V-Velocity 3.87 0.64 0.997 4.06e-5
Water Level 0.16 0.13 1.000 -3.56e-6

References

  • Dupont, F., 2001. Comparison of numerical methods for modelling ocean circulation in basins with irregular coasts. Ph.D. thesis, McGill University, Montreal.

Test Cases

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