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## Geocentric Axial Dipole Hypothesis (GAD)

## Table of Contents

^{[1]}as way of describing the time-averaged field. The hypothesis states that if the paleomagnetic field is averaged over sufficient time the field will be equivalent to that expected from a geocentric axial dipole.## Features of the GAD

The geometry of the GAD model is such that the geographic and geomagnetic poles and equators coincide (i.e., geographic latitude,λ, is equal to the time-averaged paleomagnetic latitude). The horizontal (H) and vertical (Z) components of the GAD field at a given latitude can be described by:

SHOW FIGURE OF GEOMETRY

where:

μ0 is the permeability of free space,

m is the magnetic moment of the time-averaged field,

a is the radius of the Earth.

The total field (F) is given by:

Since the tanget of the magnetic inclination, I, is Z/H, it can be shown that:

and by the definition the GAD the declination D=0 (geographic and geomagnetic poles coincide). The colatitude, p (p=90-λ) can be determined by:

The inclination-latitude relation allows paleolatitude to be determined from the mean inclinations, which is fundamental plate tectonic reconstructions and paleosecular variation studies.

The magnetic field intensity (F) of the GAD varies as a function of latitude according to:

where:

F0 is the field intensity at the equator.

SHOW FIGURE OF INTENSITY

## Testing the GAD

Given the importance of the GAD hypothesis to paleomagnetic studies it is essential that the hypothesis is tested.This article is incomplete and would benefit from your input (if you have the time).

## References

Nature,173, 1183–1184, doi: 10.1038/1731183a0.## Further Reading

McElhinny, M. (2007), Geocentric axial dipole hypothesis, inEncyclopedia of Geomagnetism and Paleomagnetism, edited by D. Gubbins and E. Herrero-Bervera, pp. 281–287, Springer, Dordrecht.## See Also

List of other relevant MagWiki pages.