This is an analytical test for the accuracy of coriolis force generated three-dimensional current and water surface slope.
Domain
- Cuboid flume
- 100,000 m length
- 5,000 m width
- 1 m height
- 45 degree latitude
![Coriolis domain Coriolis domain](/portals/55/CoriolisDomain.png)
Initial Conditions
Boundary Conditions
- No time varying boundary conditions
Results
- Run simulation to steady state
- Analytic solution for x direction flow
- Assume uniform flow
- y velocity = 0.0
- Change in u velocity with respect to x = 0.0
- Therefore
![Coriolis analytic solution x Coriolis analytic solution x](/portals/55/CoriolisAnalyticSolutionX.png)
= -2.0988e-6 m/m
- AdH computed slope = -2.154e-6
![Coriolis results elevation x Coriolis results elevation x](/portals/55/CoriolisResultsElevationX.png)
- Analytic solution for y direction flow
- Run simulation to steady state
- Assume uniform flow
- x velocity = 0.0
- Change in v velocity with respect to y = 0.0
- Therefore
![Coriolis analytic solution y Coriolis analytic solution y](/portals/55/CoriolisAnalyticSolutionY.png)
= -2.0988e-6 m/m
- AdH computed slope = -2.000e-6
![Coriolis results elevation y Coriolis results elevation y](/portals/55/CoriolisResultsElevationY.png)
- Velocity shows a curvature to the right which is again supported by Coriolis theory