Circular Basin: Difference between revisions
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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. | 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. | ||
[[Image:Grid_CB3.png|thumb|right| | [[Image:Grid_CB3.png|thumb|right|400px| Figure 1. Computational grid.]] | ||
Revision as of 22:44, 11 May 2011
UNDER CONSTRUCTION
Analytical Solution
Dupont (2001) presented an analytical solution for a closed circular domain on an f-plane, with radius , a linear bottom friction, and a spatially variable wind stress equal to , where is the gradient of the wind forcing and is the vertical coordinate. The water surface elevation solution is given by
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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.
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.