Origin of Joy's Law in the context of Near-Surface Convection on the Sun
Hannah Schunker, Asha Lakshmi K
TL;DR
The paper investigates the origin of Joy's law in the Sun, highlighting that near-surface convection likely governs active-region tilt rather than deep-seated flux tubes. It synthesizes observational results showing that the average tilt increases during emergence and that the tilt–latitude relation is primarily reflected in the north–south extent, consistent with a near-surface, Coriolis-influenced mechanism rather than a pre-emergent, deep geometric writhe. The review notes that the tilt follows a $\sin \gamma$–$\sin \lambda$ dependence and that the cycle amplitude anti-correlates with the average tilt, implying a role in dynamo regulation. It calls for more high-cadence, high-resolution surface magnetic field observations and refined statistics to disentangle the contributions of near-surface flows, flux transport, and non-linear tilt/latitude quenching to the solar cycle.
Abstract
Joy's law is a well-established statistical property of solar active regions that any theory of active region emergence must explain. This tilt angle of the active region away from an east-west alignment is a critical component for converting the toroidal magnetic field to poloidal magnetic field in some leading dynamo theories, and observations show they are important for the reversal of the sign of the global solar magnetic dipole. This review aims to synthesise observational results related to the onset of Joy's law, placing them within the broader context that describes active region emergence as a largely passive process occurring near the surface of the Sun.
