Properties of convective motions in facular regions

TL;DR

This study investigates how magnetic fields influence solar granulation in facular regions, revealing that magnetic strength affects convective velocities, reversal heights, and energy transfer in the lower solar atmosphere.

Contribution

It provides new observational insights into the dependence of convective motions and reversal heights on magnetic field strength in facular regions.

Findings

Convective velocities decrease in granules with magnetic field strength.

Reversal heights are about 100 km higher in facular regions than in quiet areas.

Magnetic fields stabilize convection and enhance energy transfer in the upper atmosphere.

Abstract

In this paper, we study the properties of solar granulation in a facular region from the photosphere up to the lower chromosphere. Our aim is to investigate the dependence of granular structure on magnetic field strength. We use observations obtained at the German Vacuum Tower Telescope (Observatorio del Teide, Tenerife) using two different instruments: Triple Etalon SOlar Spectrometer (TESOS), in the BaII 4554 A line to measure velocity and intensity variations along the photosphere; and, simultaneously, Tenerife Infrared Polarimeter (TIP-II), in the FeI 1.56 $\mu$m lines to the measure Stokes parameters and the magnetic field strength at the lower photosphere. We obtain that the convective velocities of granules in the facular area decrease with magnetic field while the convective velocities of intergranular lanes increase with the field strength. Similar to the quiet areas, there is a contrast and velocity sign reversal taking place in the middle photosphere. The reversal heights depend on the magnetic field strength and are, on average, about 100 km higher than in the quiet regions. The correlation between convective velocity and intensity decreases with magnetic field at the bottom photosphere, but increases in the upper photosphere. The contrast of intergranular lanes observed close to the disc center is almost independent of the magnetic field strength. The strong magnetic field of facular area seems to stabilize the convection and to promote more effective energy transfer in the upper layers of the solar atmosphere, since the convective elements reach larger heights.