The Formation Mechanism of Gas Giants on Wide Orbits
Sarah E. Dodson-Robinson (1), Dimitri Veras (2), Eric B. Ford (2), C., A. Beichman (3) ((1) University of Texas, (2) University of Florida, (3) NASA, Exoplanet Science Institute/Caltech)

TL;DR
This paper investigates the formation mechanisms of massive gas giants on wide orbits, concluding that gravitational instability is the most plausible process, supported by numerical simulations and stability analyses.
Contribution
It provides a comparative analysis of core accretion, scattering, and gravitational instability, demonstrating that only gravitational instability can form stable, wide-orbit gas giants.
Findings
Core accretion cannot form planets beyond 35 AU.
Planet-planet scattering does not produce stable wide-orbit systems.
High-mass disks are prone to spiral instabilities.
Abstract
The recent discoveries of massive planets on ultra-wide orbits of HR 8799 (Marois et al. 2008) and Fomalhaut (Kalas et al. 2008) present a new challenge for planet formation theorists. Our goal is to figure out which of three giant planet formation mechanisms--core accretion (with or without migration), scattering from the inner disk, or gravitational instability--could be responsible for Fomalhaut b, HR 8799 b, c and d, and similar planets discovered in the future. This paper presents the results of numerical experiments comparing the long-period planet formation efficiency of each possible mechanism in model A star, G star and M star disks. First, a simple core accretion simulation shows that planet cores forming beyond 35 AU cannot reach critical mass, even under the most favorable conditions one can construct. Second, a set of N-body simulations demonstrates that planet-planet…
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.
