Migration of Gas Giant Planets in Gravitationally Unstable Disks
arXiv:1106.1617 · doi:10.1088/2041-8205/737/2/L42
Abstract
Characterization of migration in gravitationally unstable disks is necessary to understand the fate of protoplanets formed by disk instability. As part of a larger study, we are using a 3D radiative hydrodynamics code to investigate how an embedded gas giant planet interacts with a gas disk that undergoes gravitational instabilities (GIs). This Letter presents results from simulations with a Jupiter-mass planet placed in orbit at 25 AU within a 0.14 disk. The disk spans 5 to 40 AU around a 1 star and is initially marginally unstable. In one simulation, the planet is inserted prior to the eruption of GIs; in another, it is inserted only after the disk has settled into a quasi-steady GI-active state, where heating by GIs roughly balances radiative cooling. When the planet is present from the beginning, its own wake stimulates growth of a particular global mode with which it strongly interacts, and the planet plunges inward six AU in about 10 years. In both cases with embedded planets, there are times when the planet's radial motion is slow and varies in direction. At other times, when the planet appears to be interacting with strong spiral modes, migration both inward and outward can be relatively rapid, covering several AUs over hundreds of years. Migration in both cases appears to stall near the inner Lindblad resonance of a dominant low-order mode. Planet orbit eccentricities fluctuate rapidly between about 0.02 to 0.1 throughout the GI-active phases of the simulations.
Submitted to ApJL
References in corpus (16)
- Radiation-Hydrodynamic Simulations of Collapse and Fragmentation in Massive Protostellar Cores
- The Burst Mode of Protostellar Accretion
- The properties of brown dwarfs and low-mass hydrogen-burning stars formed by disc fragmentation
- Halting Type I planet migration in non-isothermal disks
- The Two Modes of Gas Giant Planet Formation
- Characterising the Gravitational Instability in Cooling Accretion Discs
- Brown dwarf formation by gravitational fragmentation of massive, extended protostellar discs
- The Thermal Regulation of Gravitational Instabilities in Protoplanetary Disks III. Simulations with Radiative Cooling and Realistic Opacities
- Rapid inward migration of planets formed by gravitational instability
- On corotation torques, horseshoe drag and the possibility of sustained stalled or outward protoplanetary migration
- Properties of gravitoturbulent accretion disks
- Introducing a Hybrid Method of Radiative Transfer for Smoothed Particle Hydrodynamics
- Gravitational Instabilities, Chondrule Formation, and the FU Orionis Phenomenon
- The Thermal Regulation of Gravitational Instabilities in Protoplanetary Disks. IV. Simulations with Envelope Irradiation
- 3D Radiative Hydrodynamics for Disk Stability Simulations: A Proposed Testing Standard and New Results
- The potential impact of groove modes on Type II planetary migration
Cited by in corpus (39)
- Planet-disk interaction and orbital evolution
- Challenges in Forming Planets by Gravitational Instability: Disk Irradiation and Clump Migration, Accretion & Tidal Destructio
- Formation of giant planets and brown dwarfs on wide orbits
- Towards a Population Synthesis Model of Objects formed by Self-Gravitating Disc Fragmentation and Tidal Downsizing
- The near-infrared spectral energy distribution of β Pictoris b
- Fu Ori outbursts and the planet-disc mass exchange
- Does disk fragmentation prevent the formation of supermassive stars in protogalaxies?
- Interactions Between Moderate- and Long-Period Giant Planets: Scattering Experiments for Systems in Isolation and with Stellar Flybys
- Dawes Review. The tidal downsizing hypothesis of planet formation
- Planet formation from the ejecta of common envelopes
- How do Most Planets Form? -- Constraints on Disk Instability from Direct Imaging
- Chemistry in a gravitationally unstable protoplanetary disc
- The collapse of protoplanetary clumps formed through disc instability: 3D simulations of the pre-dissociation phase
- Characterization of the gaseous companion κ Andromedae b: New Keck and LBTI high-contrast observations
- The migration of gas giant planets in gravitationally unstable discs
- Tidal Downsizing model. I. Numerical methods: saving giant planets from tidal disruptions
- Radiative feedback from protoplanets in self-gravitating protoplanetary discs
- Recent developments in planet migration theory
- An alternative origin for debris rings of planetesimals
- Core-assisted gas capture instability: a new mode of giant planet formation by gravitationally unstable discs
- The Effect of Irradiation on the Jeans Mass in Fragmenting Self-Gravitating Protostellar Discs
- The Formation and Dynamics of Super-Earth Planets
- Spiral structures in gravito-turbulent gaseous disks
- Super-Earths: A New Class of Planetary Bodies
- Changes in the metallicity of gas giant planets due to pebble accretion
- Orbital Migration of Protoplanets in a Marginally Gravitationally Unstable Disk
- Tidal Downsizing Model. IV. Destructive feedback in planets
- The diverse lives of massive protoplanets in self-gravitating discs
- The evolution of self-gravitating accretion discs
- Outward migration of a giant planet with a gravitationally unstable gap edge
- Orbital migration of giant planets induced by gravitationally unstable gaps: the effect of planet mass
- Orbital Migration of Protoplanets in a Marginally Gravitationally Unstable Disk. II. Migration, Merging, and Ejection
- Modeling gravitational instabilities in self-gravitating protoplanetary disks with adaptive mesh refinement techniques
- A 3D Hydrodynamics Study of Gravitational Instabilities in a Young Circumbinary Disc
- The paradox of youth for ALMA planet candidates
- An upper limit for the growth of inner planets?
- The formation of planets by disc fragmentation
- A universal brown dwarf desert formed between planets and stars
- Triggered fragmentation in gravitationally unstable discs: forming fragments at small radii