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Research School of Astronomy and Astrophysics
Fyris Alpha Simulation Code
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2D Gresho Vortex TestsThe Gresho vortex is a 2D pattern where the cetrifugal force are matched by pressure gradients, resulting in a stable time-independent vortex. This 2D L&W test consists of single 2D vortex on a range of grid resolutions. One test models a stationary vortex, and the second test advects the vortex across three diameters. The code and configuration files plus output for Fyris to run the 2D Advection Convergence Test will be available soon. The vortex is defined here by: Initial ConditionsA vortex initially centred about (0.5, 0.5), outer radius r = 0.40 Adiabatic index Gamma = 5/3 Density = 1.0 everywhere Pressure:
Azimuthal Velocity v_phi:
The resulting 2D vorticity, V_yx (r), is
The Stationary VortexEnding Condition:
Grid:
Hydrodynamics Settings:
Errors and L1 norms are computed over a unit square centred on (0.5, 0.5) at t = 3.0. The Stationary Vortex at t = 3.0
The Moving VortexSame as the stationary vortex, with a global v_x = 1.0 drift velocity added to the whole grid, on top of the initial vortex velocity field. Ending Condition:
Grid:
The vortex drifts from the left to the right. At t = 3.0 the vortex should be centred on (3.5,0.5). Errors and L1 norms are computed over a unit square centred on the expected vortex centre at t = 3.0. ResultsThe vorticity is estimated from the discrete grid by the central finite difference: vorticity[i,j] = 0.5*{(vy[i+1, j]-vy[i-1,j])/dx - (vx[i, j+1]-vx[i,j-1])/dy} Moving Vortex at t = 3.0
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Page last updated: Wednesday, 03-Mar-2010 17:21:39 AEDT Please direct all enquiries to: Ralph.Sutherland@anu.edu.au Page authorised by: Ralph Sutherland |
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