scholarly journals Rossby Wave Instability of Thin Accretion Disks. III. Nonlinear Simulations

2001 ◽  
Vol 551 (2) ◽  
pp. 874-896 ◽  
Author(s):  
H. Li ◽  
S. A. Colgate ◽  
B. Wendroff ◽  
R. Liska
2010 ◽  
Vol 516 ◽  
pp. A31 ◽  
Author(s):  
H. Meheut ◽  
F. Casse ◽  
P. Varniere ◽  
M. Tagger

1999 ◽  
Vol 513 (2) ◽  
pp. 805-810 ◽  
Author(s):  
R. V. E. Lovelace ◽  
H. Li ◽  
S. A. Colgate ◽  
A. F. Nelson

2000 ◽  
Vol 533 (2) ◽  
pp. 1023-1034 ◽  
Author(s):  
H. Li ◽  
J. M. Finn ◽  
R. V. E. Lovelace ◽  
S. A. Colgate

2016 ◽  
Vol 823 (2) ◽  
pp. 84 ◽  
Author(s):  
Tomohiro Ono ◽  
Takayuki Muto ◽  
Taku Takeuchi ◽  
Hideko Nomura

2018 ◽  
Vol 864 (1) ◽  
pp. 70 ◽  
Author(s):  
Tomohiro Ono ◽  
Takayuki Muto ◽  
Kengo Tomida ◽  
Zhaohuan Zhu

2013 ◽  
Vol 8 (S299) ◽  
pp. 157-158
Author(s):  
Julien Faure ◽  
Sebastien Fromang ◽  
Henrik Latter

AbstractIn protoplanetary disks, the inner boundary between an MRI active and inactive region has recently been suggested to be a promising site for planet formation. A set of numerical simulations has indeed shown that vortex formation mediated by the Rossby wave instability is a natural consequence of the disk dynamics at that location. However, such models have so far considered only the case of an isothermal equation of state, while the complex thermodynamics is at the heart of how this region works. Using the Godunov code Ramses, we have performed 3D global numerical simulations of protoplanetary disks that relax the isothermal hypothesis. We find that, at the interface, the disk thermodynamics and the turbulent dynamics are intimately entwined, because of the importance of turbulent dissipation and thermal ionisation.


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