Non-linear processes in the geodynamo: palaeomagnetic evidence

Summary. Palaeomagnetic data relating to secular variation, westward drift, non-dipole field scatter, field intensities and polarity transitions are considered together in an attempt to improve our understanding of the geodynamo. An attempt is then made to interpret these data in the light of magnetohydrodynamic theory. It is suggested that polarity transitions are not characterized by significant periods of convection stasis but that dynamic processes appear to be acting throughout. Phenomena such as variable westward drift rates are explained in terms of non-linear effects relating to the magnetic field intensity. Several lines of evidence suggest that the Lorentz force is a significant body force within the Earth's core and cannot be treated as a perturbation. However, it is also suggested that the Lorentz force may become insignificant during polarity transitions, particularly during that part of a transition when the intensity is reduced and the magnetic field is predominantly non-dipolar.