Multiscale magnetic underdense regions on the solar surface: Granular and Mesogranular scales

TL;DR

This study investigates magnetic underdense regions on the solar surface across granular and mesogranular scales, revealing a multiscale turbulent convection pattern without a distinct mesogranular scale.

Contribution

It introduces a void detection method to analyze magnetic structures, demonstrating the absence of a specific mesogranular scale and supporting multiscale convection on the Sun.

Findings

Void distribution is exponential between 2 and 10 Mm.

No preferred scales found at 5-10 Mm mesogranular range.

Supports multiscale turbulent convection on the solar surface.

Abstract

The Sun is a non-equilibrium dissipative system subjected to an energy flow which originates in its core. Convective overshooting motions create temperature and velocity structures which show a temporal and spatial evolution. As a result, photospheric structures are generally considered to be the direct manifestation of convective plasma motions. The plasma flows on the photosphere govern the motion of single magnetic elements. These elements are arranged in typical patterns which are observed as a variety of multiscale magnetic patterns. High resolution magnetograms of quiet solar surface revealed the presence of magnetic underdense regions in the solar photosphere, commonly called voids, which may be considered a signature of the underlying convective structure. The analysis of such patterns paves the way for the investigation of all turbulent convective scales from granular to global. In order to address the question of magnetic structures driven by turbulent convection at granular and mesogranular scales we used a "voids" detection method. The computed voids distribution shows an exponential behavior at scales between 2 and 10 Mm and the absence of features at 5-10 Mm mesogranular scales. The absence of preferred scales of organization in the 2-10 Mm range supports the multiscale nature of flows on the solar surface and the absence of a mesogranular convective scale.