We have used a numerical scheme based on higher-order finite differences to investigate effects of adiabatic heating and viscous dissipation on 3-D rapidly rotating thermal convection in a Cartesian box with an aspect-ratio of 2x2x1. Although we omitted coupling with the magnetic field, which can play a key role in the dynamics of the Earth's core, the understanding of non-linear rotating convection including realistic thermodynamic effects is a necessary prerequisite for understanding the full complexity of the Earth's core dynamics. The system of coupled partial differential equations has been solved in terms of the principal variables vorticity ω, vector potential A and temperature T. The use of the vector potential A allows the velocity field to be calculated with one spatial differentiation in contrast to the spheroidal and toroidal function approach. The temporal evolution is governed by a coupled time-dependent system consisting of ω and T. The equations are discretized in all directions by using an eighth-order, variable spaced scheme. Rayleigh number Ra of 106, Taylor number Ta of 108 and a Prandtl number Pr of I have been employed. The dissipation number of the outer core was taken to be 0.2. A stretched grid has been employed in the vertical direction for resolving the thin shear boundary layers at the top and bottom. This vertical resolution corresponds to around 240 regularly spaced points with an eighth-order accuracy. For the regime appropriate to the Earth's outer core, the dimensionless surface temperature To takes a large value, around 4. This large value in the adiabatic heating/cooling term is found to cause stabilization of both the temperature and velocity fields.
|Original language||English (US)|
|Number of pages||23|
|Journal||Studia Geophysica et Geodaetica|
|State||Published - 2002|
Bibliographical noteFunding Information:
Acknowledgements: We thank Jakub Velímský, Ulli Hansen, Shuxia Zhang, Ladislav Hanyk, Andrei Malevsky and Bruce Buffet for fruitful discussions and encouragement in completing this work. We also acknowledge the constructive comments of an anonymous reviewer. This research has been supported by Research Project MŠMT J13/98: 113200004, the Charles University Grant 238/2001/B-GEO/MFF, the NATO Grant EST/CLG 977 093 and the Geosciences Program of the Dept. of Energy.
- 3-D convection
- Finite prandtl number
- High rayleigh number
- High-order finite differences
- Rotating fluid