Dynamo simulations show non-dipolar magnetic field strengths are comparable across dipolar and non-dipolar regimes when scaled by driving power, while the dipole component is an order of magnitude weaker in the non-dipolar regime.
Tassin , author T
3 Pith papers cite this work. Polarity classification is still indexing.
3
Pith papers citing it
representative citing papers
Top-heavy thermochemical geodynamo simulations show heterogeneous outer boundary heat flux reproduces observed longitudinal inclination anomaly variations, while elevated chemical driving reduces longitudinal structures and promotes polar radial field minima.