Abstract

Tidal dissipation in stars and planets is one of the key physical mechanisms that drive the evolution of planetary systems. It intrinsically depends on the nature of the tidal response of celestial bodies, which is directly linked to their internal structure and friction. Indeed, it is highly resonant in the case of fluids. In this work, we present a local analytical modeling of tidal gravito-inertial waves, which can be excited in stars and fluid planetary layers. This model allows us to understand the properties of their resonant dissipation as a function of the excitation frequencies, the rotation, the stratification, and the viscous and thermal properties of the studied fluid regions. Next, we introduce such a complex tidal dissipation frequency-spectra in a celestial mechanics numerical code to give a qualitative overview of its impact on the evolution of planetary systems. We consider the example of a two-body coplanar system with a punctual perturber orbiting a central fluid body. We demonstrate how the viscous dissipation of tidal waves can lead to a strongly erratic orbital evolution. Finally, we characterize such a non-regular dynamics as a function of the properties of resonances, which have been determined thanks to our local fluid model.

Highlights

  • Tidal dissipation in stars and planets is one of the key physical mechanisms that drive the evolution of planetary systems

  • [4,5] show that the Q factor of solid bodies varies smoothly with the forcing frequency. This is not the case of fluid regions, in which a resonant response to tidal perturbations is obtained [6,7,8,9]. It leads to a strong variation of the Q factor as a function of the tidal frequency because of the viscous friction and thermal diffusion acting on fluid tidal waves and to an erratic evolution of the orbital dynamics [10]

  • They are used to illustrate, through the concrete example of a planet-satellite system, how the quality factor Q and the evolution of the orbital dynamics are linked to the fluid parameters [10]

Read more

Summary

Introduction

Tidal dissipation in stars and planets is one of the key physical mechanisms that drive the evolution of planetary systems. [4,5] show that the Q factor of solid bodies varies smoothly with the forcing frequency This is not the case of fluid regions, in which a resonant response to tidal perturbations is obtained [6,7,8,9]. Using a fluid box in which rotation, stratification, viscosity and thermal diffusivity are taken into account, scaling laws describing the viscous friction applied on tidal waves are obtained They are used to illustrate, through the concrete example of a planet-satellite system, how the quality factor Q and the evolution of the orbital dynamics are linked to the fluid parameters [10]

Hydrodynamical scaling laws
Impact on tidal dynamics
Conclusions

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.