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Large-scale dynamo produced by negative magnetic eddy diffusivities.
Lanotte, A., Noullez, A., Vergassola, M. and Wirth, A. (1999) Large-scale dynamo produced by negative magnetic eddy diffusivities. Geophysical and Astrophysical Fluid Dynamics (91). pp. 131-146. DOI 10.1080/03091929908203701.
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Abstract
The existence of incompressible flow producing negative magnetic eddy diffusivities is demonstrated. This provides for a dynamo mechanism, alternative to α-type effects, requiring neither the presence of mean heliciiy nor the breaking of parity invariance. In the kinematic dynamo phase, the magnetic field grows exponentially with a growth rate proportional to the square of the wavenumber. The concrete example, analyzed by means of multiscale techniques, is a parity-invariant flow of the Taylor-Green type.
Document Type: | Article |
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Keywords: | Dynamo processes, Stability, turbulent diffusion |
Research affiliation: | OceanRep > Institute for Marine Science Kiel |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | Gordon and Breach |
Date Deposited: | 18 Feb 2008 17:24 |
Last Modified: | 28 Sep 2017 08:48 |
URI: | https://oceanrep.geomar.de/id/eprint/4271 |
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