Equivalent source magnetic dipoles revisited

Details Equivalent source magnetic dipoles revisited Equivalent source magnetic dipoles revisited

Jun 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998georl..25.2003d&link_type=abstract

Geophysical Research Letters, Volume 25, Issue 11, p. 2003-2006

Physics

8

Geomagnetism And Paleomagnetism: Spatial Variations (All Harmonics And Anomalies), Geomagnetism And Paleomagnetism: Magnetic Anomaly Modeling

Scientific paper

Equivalent point source inversion in the rectangular coordinate system has been widely used to reduce satellite magnetic data collected at different altitudes to a common elevation over small areas. This method is based on the expression of the magnetic anomaly caused by a magnetic dipole. Such an expression derived in a spherical coordinate system by von Frese et al. [1981] is found erroneous. We point out the errors in von Frese et al.'s [1981] formulas and present the correct expression for the magnetic field of a magnetic dipole in a spherical coordinate system.

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