Protoplanetary disks including radiative feedback from accreting planets
Matias Montesinos, Jorge Cuadra, Sebastian Perez, Clement Baruteau,, Simon Casassus

TL;DR
This study uses 2D hydrodynamical simulations to explore how radiative feedback from accreting planets influences protoplanetary disk evolution, thermal signatures, and observability, especially around HD 100546.
Contribution
It introduces a model incorporating planetary radiative feedback into disk simulations, revealing its impact on disk heating, accretion, and infrared emission predictions.
Findings
Planet feedback increases disk accretion rate and temperature.
Infrared spectrum of the disk is significantly modified by feedback.
Simulated feedback effects match observed luminosity of HD 100546b.
Abstract
While recent observational progress is converging on the detection of compact regions of thermal emission due to embedded protoplanets, further theoretical predictions are needed to understand the response of a protoplanetary disk to the planet formation radiative feedback. This is particularly important to make predictions for the observability of circumplanetary regions. In this work we use 2D hydrodynamical simulations to examine the evolution of a viscous protoplanetary disk in which a luminous Jupiter-mass planet is embedded. We use an energy equation which includes the radiative heating of the planet as an additional mechanism for planet formation feedback. Several models are computed for planet luminosities ranging from to Solar luminosities. We find that the planet radiative feedback enhances the disk's accretion rate at the planet's orbital radius, producing…
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