The potential impact of groove modes on Type II planetary migration
arXiv:0804.3425 · doi:10.1086/589443
Abstract
In this letter, we briefly describe the evolution of a variety of self-gravitating protoplanetary disk models that contain annular grooves (e.g. gaps) in their surface density. These grooves are inspired by the density gaps that are presumed to open in response to the formation of a giant planet. Our work provides an extension of the previously studied groove modes that are known in the context of stellar disks. The emergence of spiral gravitational instabilities (GI) is predicted via a generalized eigenvalue code that performs a linear analysis, and confirmed with hydrodynamical simulations. We find the presence of a groove drives a fast-growing two-armed mode in moderately massive disks, and extends the importance of self-gravitating instabilities down to lower disk masses than for which they would otherwise occur. We discuss the potential importance of this instability in the context of planet formation, e.g. the modification of the torques driving Type II migration.
10 pages, 5 figures. Accepted for publication in ApJ Letters. Additional color plots and movies are available at http://www.ucolick.org/~smeschia/disks.php
References in corpus (3)
Cited by in corpus (8)
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- Vortex and spiral instabilities at gap edges in three-dimensional self-gravitating disc-satellite simulations
- Edge modes in self-gravitating disc-planet interactions
- 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
- Gravitational instability of planetary gaps and its effect on orbital migration
- Instabilities at planetary gap edges in 3D self-gravitating disks