Dynamical tides in Jupiter as revealed by Juno
arXiv:2102.09072 · doi:10.3847/PSJ/abe715
Abstract
The Juno orbiter continues to collect data on Jupiter's gravity field with unprecedented precision since 2016, recently reporting a non-hydrostatic component in the tidal response of the planet. At the mid-mission perijove 17, Juno registered a Love number that is () from the theoretical hydrostatic . Here we assess whether the aforementioned departure of tides from hydrostatic equilibrium represents the neglected gravitational contribution of dynamical tides. We employ perturbation theory and simple tidal models to calculate a fractional dynamical correction to the well-known hydrostatic . Exploiting the analytical simplicity of a toy uniform-density model, we show how the Coriolis acceleration motivates the negative sign in the observed by Juno. By simplifying Jupiter's interior into a core-less, fully-convective, and chemically-homogeneous body, we calculate in a model following an polytrope equation of state. Our numerical results for the polytrope qualitatively follow the behaviour of the uniform-density model, mostly because the main component of the tidal flow is similar in each case. Our results indicate that the gravitational effect of the Io-induced dynamical tide leads to , in agreement with the non-hydrostatic component reported by Juno. Consequently, our results suggest that Juno obtained the first unambiguous detection of the gravitational effect of dynamical tides in a gas giant planet. These results facilitate a future interpretation of Juno tidal gravity data with the purpose of elucidating the existence of a dilute core in Jupiter.
22 pages, 5 figures, accepted to PSJ
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- Building the Galilean moons system via pebble accretion and migration: A primordial resonant chain
- Rotating Love: The dynamical tides of spinning Newtonian stars
- Updated Studies on Exomoons in the HD 23079 System
- Jupiter's Dynamical Love Number