Giant Planet Formation by Disk Instability: A Comparison Simulation With An Improved Radiative Scheme
Kai Cai, Megan K. Pickett, Richard H. Durisen, Anne M. Milne

TL;DR
This study compares high-resolution simulations of protoplanetary disks using different radiative schemes, finding that improved radiative modeling prevents disk fragmentation and challenges previous claims of giant planet formation via gravitational instability.
Contribution
The paper introduces an improved radiative scheme in 3D hydrodynamics simulations, demonstrating that previous models may have overestimated cooling rates leading to fragmentation.
Findings
Improved radiative scheme prevents disk fragmentation.
Previous models may have artificially accelerated cooling.
Disk remains stable with low amplitude nonaxisymmetric structures.
Abstract
There has been disagreement currently about whether cooling in protoplanetary disks can be sufficiently fast to induce the formation of gas giant protoplanets via gravitational instabilities. Simulations by our own group and others indicate that this method of planet formation does not work for disks around young, low- mass stars inside several tens of AU, while simulations by other groups show fragmentation into protoplanetary clumps in this region. To allow direct comparison in hopes of isolating the cause of the differences, we here present a high resolution three-dimensional hydrodynamics simulation of a protoplanetary disk, where the disk model, initial perturbation, and simulation conditions are essentially identical to those used in a set of simulations by Boss. As in earlier papers by the same author, Boss (2007, hereafter B07) purports to show that cooling is fast enough to…
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