Directly observing continuum emission from self-gravitating spiral waves
Cassandra Hall, Duncan Forgan, Ken Rice, Tim J. Harries, Pamela D., Klaassen, Beth Biller

TL;DR
This study uses a semi-analytic model and radiative transfer simulations to explore when self-gravitating spiral waves in discs could be observable, finding that such features require specific conditions often not met in observed systems.
Contribution
The paper introduces a simple, self-consistent model to identify parameter space where self-gravity induces detectable spiral structures in discs, clarifying the conditions for their observability.
Findings
Self-gravity requires higher disc mass than observed to produce detectable spirals.
Spiral amplitudes from self-gravity are weaker than those from tidal interactions or planet-induced waves.
Detectable self-gravitating spirals occur only in narrow parameter ranges, often not matching observed discs.
Abstract
We use a simple, self-consistent, self-gravitating semi-analytic disc model to conduct an examination of the parameter space in which self-gravitating discs may exist. We then use Monte-Carlo radiative transfer to generate synthetic ALMA images of these self-gravitating discs to determine the subset of this parameter space in which they generate non-axisymmetric structure that is potentially detectable by ALMA. Recently, several transition discs have been observed to have non-axisymmetric structure that extends out to large radii. It has been suggested that one possible origin of these asymmetries could be spiral density waves induced by disc self-gravity. We use our simple model to see if these discs exist in the region of parameter space where self-gravity could feasibly explain these spiral features. We find that for self-gravity to play a role in these systems typically requires a…
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