REVIEW 1 cited by
On the coorbital corotation torque in a viscous disk and its impact on planetary migration
Not yet reviewed by Pith; the record is open.
This paper has not been read by Pith yet. Machine review is queued; the pith claim, tier, and objections will appear here once it completes.
SPECIMEN: schema-true, not a live event
T0 review · schema-true
One-sentence machine reading of the paper's core claim.
pith:XXXXXXXX · record.json · timestamp
read the original abstract
We evaluate the coorbital corotation torque on a planet on a fixed circular orbit embedded in a viscous protoplanetary disk, for the case of a steady flow in the planet frame. This torque can be evaluated just from the flow properties at the separatrix between the librating (horseshoe) and circulating streamlines. A stationary solution is searched for the flow in the librating region. When used to evaluate the torque exerted by the circulating material of the outer and inner disk on the trapped material of the librating region, this solution leads to an expression of the coorbital corotation torque in agreement with previous estimates. An analytical expression is given for the corotation torque as a function of viscosity. Lastly, we show that additional terms in the torque expression can play a crucial role. In particular, they introduce a coupling with the disk density profile perturbation (the `dip' which surrounds the planet) and add to the corotation torque a small, positive fraction of the one-sided Lindblad torque. As a consequence, the migration could well be directed outwards in very thin disks (aspect ratio smaller than a few percent). This 2D analysis is especially relevant for mildly embedded protoplanets (sub-Saturn sized objects).
Forward citations
Cited by 1 Pith paper
-
Effects of Thermodynamics on the Concurrent Accretion and Migration of Gas Giants in Protoplanetary Disks
In 2D simulations with beta-cooling, an accreting Jupiter-mass planet migrates outward when beta is small and inward when beta exceeds the local dynamical timescale.
Discussion (0). Continue with ORCID to comment.