Circular Basin: Difference between revisions
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[[Image:Grid_CB3.png|thumb|right|600px| Figure 1. Computational grid.]] | [[Image:Grid_CB3.png|thumb|right|600px| Figure 1. Computational grid.]] | ||
The model is run to steady state from zero current and water level initial conditions with <math> W = 10^-4 \text{m}^2 \text{s}^{-2} </math>, <math> \kappa = 10^{-3} \text{s}^{-1} </math> , and | The model is run to steady state from zero current and water level initial conditions with <math> W = 10^-4 \text{m}^2 \text{s}^{-2} </math>, <math> \kappa = 10^{-3} \text{s}^{-1} </math> , and <math> f_c = 0</math>. 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 | |||
'''Table 1. General Settings for Wind-driven flow in a circular basin''' | |||
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|'''Parameter''' ||'''Value''' | |'''Parameter''' ||'''Value''' |
Revision as of 23:06, 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
(1) |
The current velocities are independent of the Coriolis parameter and are given by
(2) |
(3) |
Setup
The model is run to steady state from zero current and water level initial conditions with , , and . 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
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.