Circular Basin: Difference between revisions

From CIRPwiki
Jump to navigation Jump to search
Deleted (talk | contribs)
Deleted (talk | contribs)
Line 12: Line 12:


The current velocities are independent of the Coriolis parameter and are given by  
The current velocities are independent of the Coriolis parameter and are given by  
{{Equation| <math> u = \frac{W y }{2R\kappa </math> |2=2}}
{{Equation| <math> u = \frac{W y }{2R\kappa} </math> |2=2}}
{{Equation| <math> v = -\frac{W x }{2R\kappa </math> |2=3}}
{{Equation| <math> v = -\frac{W x }{2R\kappa} </math> |2=3}}


= Setup =
= Setup =

Revision as of 22:53, 11 May 2011

UNDER CONSTRUCTION

Analytical Solution

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

The model is run to steady state from zero current and water level initial conditions with , , and both , and . Figure 1 shows the computational grid with 5 levels of refinement from 2000 m to 125 m.

Figure 1. Computational grid.



Results

Table 2. Goodness of fit statistics for the water elevation

Statistic Value
RMSE 0.0074 m
RMAE 0.0068
R^2 0.991
Bias 0.0017 m


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

Documentation Portal