It is found that the flow divergence remained mostly negative throughout the observing period for all active regions, indicating that horizontal flows converge toward areas of strong magnetic field. It is also observed that the amplitudes of vorticity and kinetic helicity tended to increase before a series of flares occurred. After these flare episodes, the amplitudes decreased, only to rise again ahead of subsequent eruptions. This behavior was consistent across different depths below the surface, with deeper layers generally showing stronger signals. The Normalized Helicity Gradient Variance (NHGV), which captures how kinetic helicity varies with time and depth showed that NHGV typically increased at least a day before flares. Notably, about 81% of the observed flares occurred either on the day NHGV reached a local maximum or on the following day. Together, these results highlight the importance of subsurface dynamics in shaping the evolution and eruptive potential of solar active regions.
This study was published in The Astrophysical Journal (Authors: B. Lekshmi, Sushanta Tripathy, Kiran Jain, and Alexei Pevtsov)


