Hemispheric Magnetic Asymmetry and Cross-Equatorial Circulation Cells within the Sun's Near-Surface Shear Layer
Anisha Sen, S. P. Rajaguru, Ruizhu Chen, Junwei Zhao, Shukur Kholikov
TL;DR
The study tackles how cross-equatorial meridional flows in the Sun’s near-surface shear layer are modulated by hemispheric magnetic asymmetry. It uses 14 years of time-distance helioseismology with HMI and GONG data, masking active regions and computing a mass-conserving flow field to map depth-dependent patterns. The key finding is a depth-dependent circulation: upper-layer inflows toward the more active hemisphere and deeper outflows below $0.97R_{\odot}$ form cross-equatorial circulation cells with lifetimes ~2 years, while surface flux plumes move opposite to the surface flow due to deeper advection. Removing active regions reduces but does not eliminate the cross-equatorial flows, suggesting a substantial role for deeper or decayed flux in sustaining the observed dynamics, with important implications for magnetic flux transport and solar-cycle evolution.
Abstract
Using time-distance helioseismic measurements of meridional flow in the near-surface shear layer over a period of 14 years, starting from May 2010, we probe the depth structure and evolution of its cross-equatorial part. We confirm that the hemispheric magnetic asymmetry determines the amplitude and direction of such flows. Additionally, we find that these flows turn over and change direction at depths below 0.97R, forming circulation cells with lifetimes dictated again by the hemispheric magnetic imbalance, which is dominated by the occurrences of large sunspots. We also examine connections between cross-equatorial magnetic flux plumes and the flows, and discuss their implications for the equatorial flux cancellation/submergence and the poleward transport of flux.
