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Cited by 259

The DOI matches its Crossref record; 3 of the 3 references it cites were found in a registry or an index.

A Model of the Geodynamo

Busse, F. H.·2007·Geophysical Journal of the Royal Astronomical Society

Abstract

The problem of the generation of the geomagnetic field by convection in the Earth's core is considered. The complete hydromagnetic problem including the Lorentz force is solved in the case of a cylindrical configuration. Because of the dominant effect of rotation this configuration incorporates the essential features of the dynamo process in the Earth's core. The results show general agreement with the known properties of geomagnetism and the Earth's core. It is found that the toroidal field in the core is of the same order of magnitude as the poloidal field. This result is consistent with the basic assumption of theory that the Lorentz force is small compared to the Coriolis force.

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Crossref · 10.1111/j.1365-246x.1975.tb05871.x

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Metadata

Authors
Busse, F. H.
Venue
Geophysical Journal of the Royal Astronomical Society
Published
2007-04-02
Volume
42
Issue
2
Pages
437-459.
ISSN
0016-8009 (ISSN-L)
OpenAlex
W2166135358
Cited by
259
References
3
FWCI
2.63
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: A Model of the Geodynamo. https://app.cochat.ai/papers/10.1111/j.1365-246x.1975.tb05871.x
The paper
Busse, F. H. (2007). A Model of the Geodynamo. Geophysical Journal of the Royal Astronomical Society. https://doi.org/10.1111/j.1365-246x.1975.tb05871.x

Data sources

Bibliographic data: Semantic Scholar, OpenAlex, Crossref.

Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.