Volume 169, Issue 1 pp. 91-99

Representation of the main geomagnetic field using Maxwell's theory of poles

Ji-Cheng Shao

Ji-Cheng Shao

Department of Earth and Planetary Sciences, University of Tokyo, Japan

Search for more papers by this author
Yozo Hamano

Yozo Hamano

Department of Earth and Planetary Sciences, University of Tokyo, Japan

Search for more papers by this author
Michael D. Fuller

Michael D. Fuller

HIGP, SOEST, University of Hawaii at Manoa, Hawaii, USA. E-mail: [email protected]

Search for more papers by this author
First published: 22 February 2007
Citations: 1

SUMMARY

The spatio-temporal variations in the main geomagnetic field are analysed using Maxwell's source representation of the potential function defined by Maxwell's theory of poles. Maxwell sources up to order 4 are obtained for three main geomagnetic field models. The temporal variations in the main geomagnetic field are shown in terms of the variations in the parameters defined in Maxwell's source representation, for example, the Maxwell moments, the Maxwell axes, the intrinsic energy of the Maxwell source, etc. The characteristics of these variations are discussed. Applications of Maxwell's source representation of the potential function to the studies of the earth's magnetic field are suggested.

The full text of this article hosted at iucr.org is unavailable due to technical difficulties.