The general applicability of self-similar solutions for thermal disc winds
Andrew D. Sellek, Cathie J. Clarke, Richard A. Booth

TL;DR
This paper extends self-similar thermal wind models to include elevated bases and non-isothermal conditions, demonstrating their validity through hydrodynamic simulations and exploring implications for protoplanetary disc observations.
Contribution
It generalizes existing models of thermal disc winds to more realistic conditions, including elevation and temperature gradients, and validates these models with simulations.
Findings
Hydrodynamic simulations match self-similar models across various conditions.
Elevated wind bases significantly affect launch velocity and flow morphology.
Line profile widths depend on wind launch height and inclination.
Abstract
Thermal disc winds occur in many contexts and may be particularly important to the secular evolution and dispersal of protoplanetary discs heated by high energy radiation from their central star. In this paper we generalise previous models of self-similar thermal winds - which have self-consistent morphology and variation of flow variables - to the case of launch from an elevated base and to non-isothermal conditions. These solutions are well-reproduced by hydrodynamic simulations, in which, as in the case of isothermal winds launched from the mid-plane, we find winds launch at the maximum Mach number for which the streamline solutions extend to infinity without encountering a singularity. We explain this behaviour based on the fact that lower Mach number solutions do not fill the spatial domain. We also show that hydrodynamic simulations reflect the corresponding self-similar models…
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