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Magnetically Induced Rotating Rayleigh-Taylor Instability
Published on: March 3, 2017
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Kinematic dynamos in spheroidal geometries
1School of Mathematics and Statistics, University of Sydney, Sydney, New South Wales 2006, Australia.
Summary
This study numerically solves the kinematic dynamo problem for spheroidal conducting fluids, finding that strong magnetic fields can form within the spheroid, while external fields remain weak. The method uses scaling to spherical geometry for efficient computation.
Area of Science:
- Geophysics
- Plasma Physics
- Magnetohydrodynamics
Background:
- The kinematic dynamo problem describes the generation and maintenance of magnetic fields by fluid motion.
- Solving this problem for non-spherical geometries like spheroids is computationally challenging.
- Previous models often simplified the geometry or fluid properties.
Purpose of the Study:
- To numerically solve the kinematic dynamo problem for conducting spheroidal fluids.
- To investigate the influence of large aspect ratios on magnetic field generation.
- To develop a scalable computational method for spheroidal geometries.
Main Methods:
- Utilized solenoidal representations of magnetic and velocity fields using spheroidal toroidal and poloidal fields.
- Employed a non-orthogonal coordinate system and scaled the problem to spherical geometry.
- Applied spherical harmonic techniques for angular components and solved the exterior current-free condition explicitly.
Main Results:
- Developed a modified kinematic dynamo problem with anisotropic diffusion and exterior conditions.
- Found dynamo solutions for axisymmetric flows in oblate spheroids with aspect ratios up to 25.
- Observed that strong internal magnetic fields can arise, with external fields being weak and localized.
Conclusions:
- The numerical method is effective for spheroidal geometries, even with large aspect ratios.
- Fluid flow within the spheroid significantly influences the distribution of generated magnetic fields.
- The study provides insights into magnetic field generation in celestial bodies with non-spherical shapes.
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