Hydrodynamics of Embedded Planets' First Atmospheres. I. A Centrifugal Growth Barrier for 2D Flows
Chris W. Ormel, Rolf Kuiper, Ji-Ming Shi

TL;DR
This study uses 2D hydrodynamical simulations to explore how embedded planets acquire atmospheres, revealing a centrifugal growth barrier that limits atmospheric rotation and mass accumulation.
Contribution
It introduces a novel analysis of the hydrodynamics of planet atmospheres, highlighting a centrifugal barrier that constrains atmospheric growth in 2D flows.
Findings
More massive atmospheres rotate faster, limiting gas accretion.
Steady, bound flow confirmed around embedded planets.
Rotation reaches Keplerian speeds before self-gravity becomes significant.
Abstract
In the core accretion paradigm of planet formation, gas giants only form a massive atmosphere after their progenitors exceeded a threshold mass: the critical core mass. Most (exo)planets, being smaller and rock/ice-dominated, never crossed this line. Nevertheless, they were massive enough to attract substantial amounts of gas from the disc, while their atmospheres remained in pressure-equilibrium with the disc. Our goal is to characterise the hydrodynamical properties of the atmospheres of such embedded planets and their implication for their (long-term) evolution. In this paper -- the first in series -- we start to investigate the properties of an isothermal and inviscid flow past a small, embedded planet by conducting local, 2D hydrodynamical simulations. Using the PLUTO code we confirm that the flow is steady and bound. This steady outcome is most apparent for the log-polar grid…
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