Giant planet formation from disk instability; cooling and heating

dc.creatorMayer, Lucio
dc.creatorWadsley, James
dc.creatorQuinn, Thomas
dc.creatorStadel, Joachim
dc.date2003-11-03
dc.date2003-11-03
dc.date.accessioned2026-07-07T02:11:01Z
dc.date.available2026-07-07T02:11:01Z
dc.descriptionWe present the results of high resolution SPH simulations of the evolution of gravitationally unstable protoplanetary disks. We report on calculations in which the disk is evolved using a locally isothermal or adiabatic equation of state (with shock heating), and also on new simulations in which cooling and heating by radiation are explicitly modeled. We find that disks with a minimum Toomre parameter $< 1.4$ fragment into several gravitationally bound protoplanets with masses from below to a few Jupiter masses. This is confirmed also in runs where the disk is given a quiet start, growing gradually in mass over several orbital times. A cooling time comparable to the orbital time is needed to achieve fragmentation, for disk masses in the range $0.08-0.1 M_{\odot}$. After about 30 orbital times, merging between the bound condensations always leads to 2-3 protoplanets on quite eccentric orbits.
dc.description8 pages, 2 figures, to appear in the proceedings of the XIXth IAP colloquium "Extrasolar Planets: Today and Tomorrow" held in Paris, France, 2003, June 30 -- July 4, ASP Conf. Series. Images and movies of the simulations can be found at http://www.astro.washington.edu/mayer
dc.identifierhttps://arxiv.org/abs/astro-ph/0311048
dc.identifierhttp://arxiv.org/abs/astro-ph/0311048
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/6937
dc.subjectAstrophysics
dc.titleGiant planet formation from disk instability; cooling and heating
dc.typetext

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