Magnetic signals from the core of the earth and secular variation.

Journal of Geophysical Research


  • The Publications Warehouse does not have links to digital versions of this publication at this time
  • Download citation as: RIS | Dublin Core


An oscillating, radial magnetic dipole source was assumed to exist in the core of the earth, 100 km beneath the core-mantle boundary. As an approximation, electromagnetic propagation was assumed in the core in lieu of hydromagnetic propagation, which could not be used because of unknown internal fields. Using Debye potentials, the radial and horizontal components of the surface fields were calculated using various assumed conductivity parameters in the core and in the mantle. It is concluded that most spherical harmonic models of the earth's magnetic field do not include enough terms to describe properly the field of core sources with periods of tens of years. These short-period variations are especially important in describing the secular variation. Because of this, a proper description of the secular variation requires more spherical harmonic terms than are required for the field itself. Inadequate representation of short-period variations in spherical harmonic models may contribute to the rapid deterioration of predictive models. Alternatives to spherical harmonic analysis for secular variation should be investigated; regardlesss of the method used, a much greater spatial distribution of high quality secular variation data is needed. -Author

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Magnetic signals from the core of the earth and secular variation.
Series title Journal of Geophysical Research
Volume 86
Issue B9
Year Published 1981
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Journal of Geophysical Research
First page 7957
Last page 7965
Google Analytic Metrics Metrics page
Additional metadata about this publication, not found in other parts of the page is in this table