Active regions and the large-scale magnetic field of solar cycle 24
This study utilizes surface flux transport modeling and randomized simulations to demonstrate that the non-random longitudinal distribution of active regions, particularly recurrent flux emergence in the southern hemisphere, significantly reinforced the large-scale equatorial magnetic field during the declining phase of solar cycle 24, while also showing that incorporating both axial and equatorial dipole components provides better constraints for model optimization than using the axial dipole alone.