http://arxiv.org/abs/2305.07929
Disk winds are thought to play a critical role in the evolution and dispersal of protoplanetary disks. The primary diagnostic of this physics is emission from the wind, especially in the low-velocity component of the [O I] $\lambda6300$ line. However, the interpretation of the line is usually based on spectroscopy alone, which leads to confusion between magnetohydrodynamic winds and photoevaporative winds. Here, we report that in high-resolution VLT/MUSE spectral mapping of TW~Hya, 80 % of the [O ] emission is confined to within 1 AU radially from the star. A generic model of a magnetothermal wind produces [O I] emission at the base of the wind that broadly matches the flux and the observed spatial and spectral profiles. The emission at large radii is much fainter that predicted from models of photoevaporation, perhaps because the magnetothermal wind partially shields the outer disk from energetic radiation from the central star. This result calls into question the assumed importance of photoevaporation in disk dispersal predicted by models.
M. Fang, L. Wang, G. Herczeg, et. al.
Tue, 16 May 23
11/83
Comments: Accepted for publication in Nature Astronomy