Vortex Formation and Evolution in Planet Harboring Disks under Thermal Relaxation
A. Lobo Gomes, H. Klahr, A. L. Uribe, P. Pinilla, C. Surville

TL;DR
This study investigates how radial buoyancy influences vortex formation and evolution in planet-hosting disks using hydrodynamical simulations, revealing effects on vortex strength, generation, and lifetime.
Contribution
It demonstrates that radial buoyancy weakens vortices and causes a two-generation vortex formation process, with implications for observed vortex locations in disks.
Findings
Radial buoyancy leads to smoother planetary gaps and weaker vortices.
Two generations of vortices form, with the second triggered by surface density enhancements.
Vortex lifetimes vary nonmonotonically with thermal relaxation timescales.
Abstract
We study the evolution of planet-induced vortices in radially stratified disks, with initial conditions allowing for radial buoyancy. For this purpose we run global two dimensional hydrodynamical simulations, using the PLUTO code. Planet-induced vortices are a product of the Rossby wave instability (RWI) triggered in the edges of a planetary gap. In this work we assess the influence of radial buoyancy for the development of the vortices. We found that radial buoyancy leads to smoother planetary gaps, which generates weaker vortices. This effect is less pronounced for locally isothermal and quasi-isothermal (very small cooling rate) disks. We observed the formation of two generations of vortices. The first generation of vortices is formed in the outer wall of the planetary gap. The merged primary vortex induces accretion, depleting the mass on its orbit. This process creates a surface…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
