Einstein once cited the origin of the Earth's magnetic field as one of the fundamental unsolved problems of physics. Although there has been progress on paper, experimental models have been elusive until now.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Gailitis, A. et al. Phys. Rev. Lett. 84, 4365– 4368 (2000).
Müller, U. & Stieglitz, R. Workshop on Homogeneous Dynamos Forschungszentrum Karlsruhe, 20 –22 March 2000.
Larmor, J. Br. Assoc. Adv. Sci. Rep. 159–160 ( 1919).
Bullard, E. C. Proc. Camb. Phil. Soc. 51, 744–760 (1955).
Lowes, F. J. & Wilkinson, I. Nature 198, 1158–1160 (1963).
Lowes, F. J. & Wilkinson, I. Nature 219, 717–718 (1968).
Cowling, T. G. Mon. Not. R. Astron. Soc. 94, 39–48 (1934).
Busse, F. H. Annu. Rev. Fluid Mech. 32, 383–408 (2000).
Tilgner, A. Phys. Earth Planet. Int. 117, 171– 177 (2000).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Jackson, A. Critical time for fluid dynamos. Nature 405, 1003–1004 (2000). https://doi.org/10.1038/35016667
Issue Date:
DOI: https://doi.org/10.1038/35016667