Abstract

ABSTRACT Photoevaporation driven by high-energy radiation from the central star plays an important role in the evolution of protoplanetary discs. Photoevaporative winds have been unambiguously detected through blue-shifted emission lines, but their detailed properties remain uncertain. Here we present a new empirical approach to make observational predictions of these thermal winds, seeking to fill the gap between theory and observations. We use a self-similar model of an isothermal wind to compute line profiles of several characteristic emission lines (in particular the [Ne ii] line at 12.81 μm, and optical forbidden lines such as [O i] 6300 Å and [S ii] 4068/4076 Å), studying how the lines are affected by parameters such as the gas temperature, disc inclinations, and density profile. Our model successfully reproduces blue-shifted lines with $v_{\rm peak} \lesssim 10$ km s−1, which decrease with increasing disc inclination. The line widths increase with increasing disc inclinations and range from $\Delta v\sim 15\text{ to }30$ km s−1. The predicted blue-shifts are mostly sensitive to the gas sound speed (and therefore the temperature). The observed [Ne ii] line profiles are consistent with a thermal wind and point towards a relatively high sound speed, as expected for extreme-UV photoevaporation. However, the observed [O i] line profiles require lower temperatures, as expected in X-ray photoevaporation, and show a wider scatter that is difficult to reconcile with a single wind model; it seems likely that these lines trace different components of a multiphase wind. We also note that the spectral resolution of current observations remains an important limiting factor in these studies, and that higher resolution spectra are required if emission lines are to further our understanding of protoplanetary disc winds.

Highlights

  • Protoplanetary discs are the sites of planet formation, and these discs play a critical role in the formation and early evolution of planetary systems

  • Determining line parameters by fitting Gaussian line profiles introduces further uncertainties, as our models have shown that winds are expected to result in line profiles that are not well fitted by a Gaussian profile. These factors limit our ability to discriminate between models using current data, and our results show that significantly higher spectral resolution (R 100 000) is required if we are to use these line profiles to measure the properties of disc winds in greater detail

  • We have presented a new approach to calculate observable diagnostics of photoevaporative disc winds

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Summary

Introduction

Protoplanetary discs are the sites of planet formation, and these discs play a critical role in the formation and early evolution of planetary systems. Planets form in, and from, evolving discs, but consideration of the mass budget shows that only a small fraction of the disc mass ends up in planets; disc evolution is primarily driven by a combination of accretion and mass-loss Observations show that disc winds are characterized by two components: a high-velocity ( 100 km s−1) component associated with magnetically launched winds/jets, and a low-velocity. Forbidden line diagnostics of photoevaporative disc winds 2933. We focus on thermal winds, which in this context are invariably driven by photoevaporation. The thermal energy of the heated gas is sufficient for it to escape the star’s gravitational potential, and the result is a thermally launched, pressure-driven flow. The characteristic (‘gravitational’) radius for disc photoevaporation is

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