2008
DOI: 10.1016/j.crhy.2008.07.003
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Geomagnetism and the dynamo: where do we stand?

Abstract: We review recent developments both in the observation of the Earth's magnetic field (from the short, human life timescale, to the long, geological timescale) and in the modelling of its origin (using the numerical or the experimental approach). We attempt a confrontation of these results, coming from very different fields, and show how, when combined, they can yield a better understanding of the Earth's core dynamics. We assume prior knowledge of dynamo theory, but not of geophysics. To cite this article: E.

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Cited by 12 publications
(6 citation statements)
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References 43 publications
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“…One can show in a similar manner that for a subcritical bifurcation with a normal form given by (4)(5), the probability P (X) to meet a given value is…”
Section: Feedback and Couplingmentioning
confidence: 91%
See 1 more Smart Citation
“…One can show in a similar manner that for a subcritical bifurcation with a normal form given by (4)(5), the probability P (X) to meet a given value is…”
Section: Feedback and Couplingmentioning
confidence: 91%
“…In the absence of noise (ξ ≡ 0), solutions to (4)(5) are: the trivial X = 0 (stable for µ < 0 unstable otherwise), and the four roots of µ + αX 2 − X 4 , for −α 2 /4 µ < 0. Two of these are unstable, the two others being stable (subcritical branch) and continuous for µ 0.…”
Section: Feedback and Couplingmentioning
confidence: 99%
“…The hydrodynamics of conducting fluids is of great importance in many terrestrial and astrophysical phenomena. Examples include the generation of magnetic fields via dynamo action in the interstellar medium, stars, and planets [1,2,3,4,5,6,7,8,9,10,11], and liquid-metal systems [12,13,14,15,16,17,18] that are studied in laboratories. The flows in such settings, which can be described at the simplest level by the equations of magnetohydrodynamics (MHD), are often turbulent [5].…”
Section: Introductionmentioning
confidence: 99%
“…This fascination is not restricted to fluid turbulence, for which we use the Navier-Stokes equation, but it also extends to other forms of turbulence, such as that in conducting fluids, for which we use the equations of magnetohydrodynamics (MHD) [3,4,5,6,7,8] and on which we concentrate here. The flows of such conducting fluids is often turbulent in a variety of physical settings, including liquid-metal flows in terrestrial laboratories and planetary interiors [9,10,11,12,13,14,15], in stars such as the sun [3,4,6,7], in the solar wind [16,17], and in the interstellar medium [4,5,6].…”
Section: Introductionmentioning
confidence: 99%