Gap formation and stability in non-isothermal protoplanetary discs
Robert Les, Min-Kai Lin

TL;DR
This study investigates how non-isothermal conditions affect vortex formation and stability at planetary gap edges in protoplanetary discs, revealing that cooling times influence vortex lifetime and characteristics.
Contribution
It extends the theory of vortex formation to non-isothermal discs by incorporating a simple cooling function, analyzing its impact on vortex stability and lifetime through numerical simulations.
Findings
Increasing cooling times decrease perturbation growth rates.
Vortex lifetimes peak at an optimal cooling timescale.
Vortex characteristics depend on the cooling parameter eta.
Abstract
Several observations of transition discs show lopsided dust-distributions. A potential explanation is the formation of a large-scale vortex acting as a dust-trap at the edge of a gap opened by a giant planet. Numerical models of gap-edge vortices have thus far employed locally isothermal discs, but the theory of this vortex-forming or `Rossby wave' instability was originally developed for adiabatic discs. We generalise the study of planetary gap stability to non-isothermal discs using customised numerical simulations of disc-planet systems where the planet opens an unstable gap. We include in the energy equation a simple cooling function with cooling timescale , where is the Keplerian frequency, and examine the effect of on the stability of gap edges and vortex lifetimes. We find increasing lowers the growth rate of non-axisymmetric…
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