Internal Waves and Tides in Stars and Giant Planets

Author(s):  
Gordon I. Ogilvie
2013 ◽  
Vol 62 ◽  
pp. 323-362 ◽  
Author(s):  
S. Mathis ◽  
L. Alvan ◽  
F. Remus

2010 ◽  
Vol 128 (4) ◽  
pp. 2386-2386
Author(s):  
John A. Colosi ◽  
Brian Dushaw ◽  
Rex K. Andrew ◽  
Lora J. Van Effelen ◽  
Matthew A. Dzieciuch ◽  
...  

2011 ◽  
Vol 130 (4) ◽  
pp. 2556-2556
Author(s):  
John Colosi ◽  
Brian Dushaw ◽  
Lora Van Uffelen ◽  
Matt Dzieciuch ◽  
Bruce Cornuelle ◽  
...  

1995 ◽  
Vol 98 (5) ◽  
pp. 2863-2863
Author(s):  
Albert J. Plueddemann ◽  
James F. Lynch

2009 ◽  
Vol 126 (4) ◽  
pp. 2285
Author(s):  
Chi-Fang Chen ◽  
Yung-Sheng Linus Chiu ◽  
Yuan-Ying Chang

2020 ◽  
Vol 493 (4) ◽  
pp. 5788-5806
Author(s):  
C M Pontin ◽  
A J Barker ◽  
R Hollerbach ◽  
Q André ◽  
S Mathis

ABSTRACT Recent observations of Jupiter and Saturn suggest that heavy elements may be diluted in the gaseous envelope, providing a compositional gradient that could stabilize ordinary convection and produce a stably stratified layer near the core of these planets. This region could consist of semiconvective layers with a staircase-like density profile, which have multiple convective zones separated by thin stably stratified interfaces, as a result of double-diffusive convection. These layers could have important effects on wave propagation and tidal dissipation that have not been fully explored. We analyse the effects of these layers on the propagation and transmission of internal waves within giant planets, extending prior work in a local Cartesian model. We adopt a simplified global Boussinesq planetary model in which we explore the internal waves in a non-rotating spherical body. We begin by studying the free modes of a region containing semiconvective layers. We then analyse the transmission of internal waves through such a region. The free modes depend strongly on the staircase properties, and consist of modes with both internal and interfacial gravity wave-like behaviour. We determine the frequency shifts of these waves as a function of the number of steps to explore their potential to probe planetary internal structures. We also find that wave transmission is strongly affected by the presence of a staircase. Very large wavelength waves are transmitted efficiently, but small-scale waves are only transmitted if they are resonant with one of the free modes. The effective size of the core is therefore larger for non-resonant modes.


1997 ◽  
Vol 102 (C1) ◽  
pp. 1073-1089 ◽  
Author(s):  
Murray D. Levine ◽  
Laurie Padman ◽  
Robin D. Muench ◽  
James H. Morison

1981 ◽  
Vol 134 (8) ◽  
pp. 675 ◽  
Author(s):  
S.V. Vorontsov ◽  
V.N. Zharkov

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