Earth's magnetic poles are maintained and positioned by convection currents in the liquid outer core
Earth's magnetic field is widely understood and modeled as being generated and maintained by convection currents and fluid motion within the liquid outer core (the geodynamo).
The claim aligns with well-established geophysics regarding the geodynamo, supported by simulation and theoretical papers in the literature showing that outer core convection generates Earth's magnetic field.
Alka Tripathy-Lang. How Geodynamo Models Churn the Outer Core. 2021. https://doi.org/10.1029/2021eo154727
Simulations of Earth's outer core successfully reproduce magnetic fields using geodynamo models.
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Thomas Frasson. Heterogeneous heat flux from mantle convection simulations : impact on the geodynamo and magnetic reversals. https://doi.org/10.70675/c4656d27zcfddz4b18z9500z287025e94346
The terrestrial magnetic field is generated and maintained by the convection of liquid iron in the core through a dynamo effect.
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