2003
DOI: 10.1086/367555
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Orbital Migration and Mass Accretion of Protoplanets in Three‐dimensional Global Computations with Nested Grids

Abstract: We investigate the evolution of protoplanets with different masses embedded in an accretion disk, via global fully three-dimensional hydrodynamical simulations. We consider a range of planetary masses extending from one and a half Earth's masses up to one Jupiter's mass, and we take into account physically realistic gravitational potentials of forming planets. In order to calculate accurately the gravitational torques exerted by disk material and to investigate the accretion process onto the planet, the flow d… Show more

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Cited by 243 publications
(289 citation statements)
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References 30 publications
(59 reference statements)
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“…8), in good agreement with Nelson et al (2000), D'Angelo & Kley (2003) and a simple estimate of the viscous time scale. Note that due to the initial gap clearing phase the planet has already migrated to r = 9.43 after 535 orbits.…”
Section: Planet Calibration Run: Modelsupporting
confidence: 81%
“…8), in good agreement with Nelson et al (2000), D'Angelo & Kley (2003) and a simple estimate of the viscous time scale. Note that due to the initial gap clearing phase the planet has already migrated to r = 9.43 after 535 orbits.…”
Section: Planet Calibration Run: Modelsupporting
confidence: 81%
“…The empirical formula for the accretion rate based on local two-dimensional isothermal hydrodynamic simulations (TW02) can be different from that derived based on more realistic simulations including, for example, three-dimensional accretion flow ( D'Angelo et al 2003;Bate et al 2003), a nonisothermal equation of state (TW02), and a magnetic field (Machida et al 2006). The modification would change the form of div , which would yield quantitatively different results.…”
Section: Remarks On the Uncertainties In The Modelmentioning
confidence: 99%
“…Subsequent eccentricity damping in the protoplanetary disk may also occur. The distribution of final orbital sizes may result from inward migration and mutual interactions among the planets, in a race against the dissipation of the protoplanetary disk, leaving the planets frozen in their tracks (Armitage et al 2003;Trilling et al 2002;D'Angelo et al 2003; Thommes & Lissauer 2003;Ida & Lin 2004;Alibert et al 2005). …”
Section: Introductionmentioning
confidence: 99%