Stable magnetic fields and changing starspots on Vega -- An ultra-deep decadal survey at Pic du Midi and OHP
T. Böhm, M. Holschneider, P. Petit, F. Lignières, F. Paletou, C. P. Folsom, M. Rainer
TL;DR
This study presents an ultra-deep, decadal survey of Vega using high-resolution spectroscopy and spectropolarimetry from SOPHIE and NARVAL/NEO-NARVAL/TBL to map surface magnetism via Zeeman-Doppler Imaging and to reconstruct brightness spot distributions. It finds a long-lived, stable oblique dipole with a polar radial-field patch, suggesting a fossil magnetic component, alongside smaller-scale magnetic features that persist yet may be time-variable. In contrast, brightness spots migrate across years with constant contrast, indicating dynamic surface activity that does not straightforwardly correlate with the large-scale magnetic field. The results point to a two-component magnetism model in Vega, combining a fossil field with a dynamo-generated equatorial component, and have important implications for understanding magnetic fields in radiative envelopes of A-type stars.$P = 0.6705 \,\pm\,0.0019$ d and $P \approx 0.678$ d are used to phase the data and compare across epochs, highlighting the decadal stability of the large-scale field against evolving surface activity.
Abstract
Monitoring magnetic and activity variations in A- and B-type stars with ultra-weak magnetic fields is essential to understand the origin and evolution of these fields in this region of the HR diagram, with Vega standing as the prototype of this category. We collected high-resolution spectroscopic and spectropolarimetric data with SOPHIE (OHP, 2018) and with NARVAL/NEO-NARVAL (TBL, 2018, 2023, and 2024), yielding a total of 13108 individual spectra. Magnetic field maps were reconstructed using the Zeeman-Doppler Imaging method, while brightness maps were derived with a dedicated code developed for this purpose. The average magnetic field confirms a negative radial-field spot at the pole with stable strength, while the maps reveal the long-term stability of an oblique dipole together with smaller magnetic structures consistently detected across observing epochs. In contrast, brightness maps show strong variations in the location of surface spots on timescales of years, possibly shorter, although the spot contrast remains nearly unchanged between 2012, 2018, 2023, and 2024, with a normalized spectral amplitude of 0.0003. No direct correlation between magnetic and brightness features could be established in the simultaneous SOPHIE and NARVAL dataset of 2018. These results suggest that Vega hosts both a persistent fossil magnetic field and a dynamo-generated component, most likely concentrated in equatorial regions.
