Affiliation:
1. ERDW, Institut für Geophysik, ETH Zurich, Sonneggstrasse 5, Zürich 8092, Switzerland
2. Department of Mathematical Sciences, Durham University, Durham DH1 3LE, UK
Abstract
Planetary magnetic fields are generated by the motion of conductive fluid in the planet's interior. Complex flows are not required for dynamo action; simple flows have been shown to act as efficient kinematic dynamos, whose physical characteristics are more straightforward to study. Recently, Chen
et al
. (2018,
J. Fluid Mech.
839
, 1–32. (
doi:10.1017/jfm.2017.924
)) found the optimal, unconstrained kinematic dynamo in a sphere, which, despite being of theoretical importance, is of limited practical use. We extend their work by restricting the optimization to three simple two-mode axisymmetric flows based on the kinematic dynamos of Dudley & James (1989,
Proc. R. Soc. Lond. A
425
, 407–429. (
doi:10.1098/rspa.1989.0112
)). Using a Lagrangian optimization, we find the smallest critical magnetic Reynolds number for each flow type, measured using an enstrophy-based norm. A Galerkin method is used, in which the spectral coefficients of the fluid flow and magnetic field are updated in order to maximize the final magnetic energy. We consider the
t
0
1
s
0
1
,
t
0
1
s
0
2
and
t
0
2
s
0
2
flows and find enstrophy-based critical magnetic Reynolds numbers of 107.7, 142.4 and 125.5 (13.7, 19.6 and 16.4, respectively, with the energy-based definition). These are up to four times smaller than the original flows. These simple and efficient flows may be used as benchmarks in future studies.
Funder
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Subject
General Physics and Astronomy,General Engineering,General Mathematics
Reference28 articles.
1. On the genesis of the Earth's magnetism
2. How could a rotating body such as the Sun become a magnet?;Larmor J;Rep. Brit. Assoc.,1919
3. Homogeneous dynamos and terrestrial magnetism;Bullard EC;Proc. R. Soc. Lond. A,1954
4. Roberts GO. 1971 Reported by P.H. Roberts in World magnetic surveys 1957–1969 (ed. AJ Zmuda) pp. 123–131. Paris: International Union of Geodesy and Geophysics Publication Office.
5. Numerical solutions of the kinematic dynamo problem;Gubbins D;Proc. R. Soc. Lond. A,1973
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