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Journal ArticleDOI

Dynamo Scaling Laws and Applications to the Planets

Ulrich R. Christensen
- 01 May 2010 - 
- Vol. 152, Iss: 1, pp 565-590
TLDR
The scaling laws for planetary dynamos relate the characteristic magnetic field strength, characteristic flow velocity and other properties to primary quantities such as core size, rotation rate, electrical conductivity and heat flux as discussed by the authors.
Abstract
Scaling laws for planetary dynamos relate the characteristic magnetic field strength, characteristic flow velocity and other properties to primary quantities such as core size, rotation rate, electrical conductivity and heat flux. Many different scaling laws have been proposed, often relying on the assumption of a balance of Coriolis force and Lorentz force in the dynamo. Their theoretical foundation is reviewed. The advent of direct numerical simulations of planetary dynamos and the ability to perform them for a sufficiently wide range of control parameters allows to test the scaling laws. The results support a magnetic field scaling that is not based on a force balance, but on the energy flux available to balance ohmic dissipation. In its simplest form, it predicts a field strength that is independent of rotation rate and electrical conductivity and proportional to the cubic root of the available energy flux. However, rotation rate controls whether the magnetic field is dipolar or multipolar. Scaling laws for velocity, heat transfer and ohmic dissipation are also discussed. The predictions of the energy-based scaling law agree well with the observed field strength of Earth and Jupiter, but for other planets they are more difficult to test or special pleading is required to explain their field strength. The scaling law also explains the very high field strength of rapidly rotating low-mass stars, which supports its rather general validity.

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References
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Book

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TL;DR: In this paper, a thermal model of the Earth is presented, based on a geophysical model of an isotropic solid and a geomagnetic field model of a geodesic shell.
Journal ArticleDOI

A three-dimensional self-consistent computer simulation of a geomagnetic field reversal

TL;DR: In this article, a three-dimensional, self-consistent numerical model of the geodynamo is described, which maintains a magnetic field for over 40,000 years, including a successful reversal of the dipole moment.
Journal ArticleDOI

Scaling properties of convection-driven dynamos in rotating spherical shells and application to planetary magnetic fields

TL;DR: In this paper, an extensive set of dynamo models in rotating spherical shells, varying all relevant control parameters by at least two orders of magnitude, were studied and their scaling laws were established.
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