Hostname: page-component-7479d7b7d-68ccn Total loading time: 0 Render date: 2024-07-10T15:29:32.848Z Has data issue: false hasContentIssue false

Dynamo action associated with random inertial waves in a rotating conducting fluid

Published online by Cambridge University Press:  29 March 2006

H. K. Moffatt
Affiliation:
Department of Applied Mathematics and Theoretical Physics, Silver Street, Cambridge

Abstract

It is shown that a random superposition of inertial waves in a rotating conducting fluid can act as a dynamo, i.e. can systematically transfer energy to a magnetic field which has no source other than electric currents within the fluid. Dynamo action occurs provided the statistical properties of the velocity field lack reflexional symmetry, and this occurs when conditions are such that there is a net energy flux (positive or negative) in the direction of the rotation vector Ω.

If the magnetic field grows from an infinitesimal level, then the mode of maximum growth rate dominates before the back-reaction associated with the Lorentz force becomes significant. This mode is first determined, and then the back-reaction associated with it alone is analysed. It is shown that the magnetic energy grows exponentially during the stage when the Lorentz forces are negligible, then reaches a maximum depending on the values of the parameters \[ R_m = u_0 l/\lambda,\quad Q = \Omega l^2/\lambda, \] (u0 = initial r.m.s. velocity, l = length scale characteristic of the velocity field, λ = magnetic diffusivity) and ultimately decays as t−1 (equation (5.15)). This decay is coupled with a decay of the velocity field due to ohmic dissipation, and it occurs because there is no external source of energy for the fluid motion.

Type
Research Article
Copyright
© 1970 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Chandrasekhar, S. 1961 Hydrodynamic and Hydromagnetic Stability. Oxford University Press.
Childress, S. 1969 A class of solutions of the magnetohydrodynamic dynamo problem. Reprinted from The Application of Modern Physics to the Earth and Planetary Interiors (ed. S. K. Runcorn). New York: Interscience.
Gradshteyn, I. S. & Rijzhik, I. M. 1965 Tables of Integrals, Series and Products. New York: Academic.
Greenspan, H. P. 1968 The Theory of Rotating Fluids. Cambridge University Press.
Hide, R. & Malin, S. R. C. 1970 Novel correlations between global features of the Earth's gravitational and magnetic fields. Nature, 225, 605.Google Scholar
Lehnert, B. 1954 Magnetohydrodynamic waves under the action of the Coriolis force. Astrophys. J. 119, 647.Google Scholar
Moffatt, H. K. 1970 Turbulent dynamo action at low magnetic Reynolds number. J. Fluid Mech. 41, 43.
Roberts, G. O. 1969 Periodic dynamos. Ph.D. thesis, Cambridge University.
Roberts, P. H. 1967 An introduction to Magnetohydrodynamics. London: Longmans.
Steenbeck, M., Krause, F. & Radler, K. H. 1966 Berechnung der mittleren Lorentz-Feldstärke v B für ein elektrisch leitendes Medium in turbulenter, durch Coriolis-Kräfte beeinflusster Bewegung. Z. Naturf. 21 a, 369.Google Scholar