Geomagnetic dipole stability and zonal flows controlled by mantle heat flux heterogeneities

TL;DR

This study investigates how mantle heat flux heterogeneities influence Earth's geodynamo, revealing their role in magnetic field reversals and transitions between dipolar and multipolar states through advanced simulations.

Contribution

It demonstrates that mantle heat flux heterogeneities can induce magnetic field reversals and multipolar dynamos, advancing understanding of Earth's magnetic history with realistic mantle convection parameters.

Findings

Heat flux heterogeneities favor multipolar dynamos.

Reversals are triggered by equatorial symmetry breaking or eastward zonal flows.

Strong field models are less sensitive to heterogeneities.

Abstract

This work aims at acquiring a more complete understanding of how lateral heterogeneities of the CMB heat flux affect the geodynamo while other relevant parameters are pushed towards realistic values. For this purpose, we ran geodynamo simulations with degree 1 and 2 spherical harmonic patterns of heat flux at the CMB. Several geodynamo models are used, ranging from standard numerical dynamos to more extreme parameters, including strong field cases and turbulent cases. We show that heat flux heterogeneities with amplitudes compatible with our knowledge of mantle convection history can favour multipolar dynamos. The multipolar transition is associated with a disruption of westward flows either through eastward thermal winds or through a loss of equatorial symmetry. Strong field dynamo models are found to have larger westward flows and are less sensitive to heat flux heterogeneities. Furthermore, we find that the dipolar fraction of the magnetic field correlates with $M_{Za}^*=\dfrac{\Lambda_{Za}}{Rm_{Za}^2}$ where $\Lambda_{Za}$ is the zonal antisymmetric Elsasser number and $Rm_{Za}$ is the zonal antisymmetric magnetic Reynolds number. Importantly, $M_{Za}^*$ estimated for the Earth's core is consistent with a reversing dipolar magnetic field. Within the range of $M_{Za}^*$ susceptible to reversals, breaking the equatorial symmetry or forcing eastward zonal flows through an equatorial cooling of the core consistently triggers reversals or a transition towards multipolar dynamos in our simulations. Our results support that time variations of heat-flux heterogeneities driven by mantle convection through Earth's history are capable of inducing the significant variations in the reversal frequency observed in the palaeomagnetic record.