Origin of the asymmetric gas distribution near the co-orbital Lagrange points of an embedded planet
Agustin Heron, Cristobal Petrovich, Pablo Ben\'itez-Llambay, Juan Garrido-Deutelmoser

TL;DR
This study uses hydrodynamic simulations to reveal that the asymmetry in gas distribution near co-orbital Lagrange points of an embedded planet is controlled by the radial temperature gradient, influencing observed disk features.
Contribution
It demonstrates that the gas asymmetry is governed by the radial temperature gradient and links the azimuthal positions of Lagrange points to disk pressure scale height, providing new insights into planet-disk interactions.
Findings
Asymmetry is controlled by the sign of the radial temperature gradient.
Azimuthal locations of L4 and L5 deviate from classical predictions based on disk scale height.
Large-amplitude structures are associated with planets opening shallow gaps.
Abstract
Hydrodynamic simulations of planet-disk interactions often show material accumulation near the co-orbital Lagrange points and -- features that may correspond to observed crescents in protoplanetary disks. Intriguingly, these simulations also show an asymmetrical distribution of gas between and , whose physical origin is not yet understood and could allow to further constrain the inner workings of planet-disk interactions. We performed 2D hydrodynamic simulations of a single, non-migrating planet embedded in a gaseous disk to investigate this effect. We find that the asymmetry is solely controlled by the sign of the radial temperature gradient with positive gradients enhancing the accumulation at and negative ones enhancing . A symmetric distribution is recovered on globally isothermal disks. Furthermore, we find that the azimuthal locations of and…
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