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On the dynamical origins of retrograde Jupiter Trojans and their connection to high-inclination TNOs

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Abstract

Over the course of the last decade, observations of highly inclined (orbital inclination i > 60\(^\circ \)) trans-Neptunian objects (TNOs) have posed an important challenge to current models of solar system formation (Levison et al. in Icarus 196(1):258–273, 2008; Nesvorný in Astron J 150:73, 2015). These remarkable minor planets necessitate the presence of a distant reservoir of strongly out-of-plane TNOs, which itself requires some dynamical production mechanism (Gladman et al. in Astron J Lett 697:L91–L94, 2009; Gomes et al. in Icarus 258:37–49, 2015; Batygin and Brown in Astrophys J 833(1):L3, 2016). A notable recent addition to the census of high-i minor bodies in the solar system is the retrograde asteroid 514107 Ka’epaoka’awela, which currently occupies a 1:-1 mean motion resonance with Jupiter at i = 163\(^\circ \) (Wiegert et al. in Nature 543:687–689, 2017). In this work, we delineate a direct connection between retrograde Jupiter Trojans and high-i Centaurs. First, we backpropagate a large sample of clones of Ka’epaoka’awela for 100 Ma numerically and demonstrate that long-term stable clones tend to decrease their inclination steadily until it concentrates between 90\(^\circ \) and 135\(^\circ \), while their eccentricity and semi-major axis increase, placing many of them firmly into the trans-Neptunian domain. Importantly, the clones show significant overlap with the synthetic high-i Centaurs generated in Planet 9 studies (Batygin et al. in Phys Rep 805:1–53, 2019), and hint at the existence of a relatively prominent, steady-state population of minor bodies occupying polar trans-Saturnian orbits. Second, through direct numerical forward modeling, we delineate the dynamical pathway through which conventional members of the Kuiper Belt’s scattered disk population can become retrograde Jovian Trojan resonators in the presence of Planet 9.

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Notes

  1. We note that in chaotic dynamics, forward and backward integrations are statistically equivalent.

  2. We parallelized our simulation into 62 subprocesses with 100 test particles each. The cloning is done inside these sub-simulations, such that whenever the resampling is triggered by having less than 25 of the initial 100 particles left, the leftover objects are (randomly assigned) parents for as many clones that are needed to reach 100 objects again.

  3. The Lyapunov time is estimated with the REBOUND software containing the Sun, the four outer planets and Ka’epaoka’awela. The IAS15 integrator (Rein and Spiegel 2015) is used with a time step of 100 days.

  4. Although the initial conditions for the TNO population have been taken from a simulation with Planet 9, the particles have been propagated forward in time without Planet 9, as we do not expect the planet to have a significant influence on the test particles’ trajectories once they begin their journey to the inner planets. The observation that these high-inclination TNOs exist in the first place is independent of their assumed method of generation: We merely show that their population could explain the presence of polar SSSBs co-orbital to the giant planets.

  5. We performed the same simulation without Planet 9 and reach comparable results. This is expected since the particles observed are far enough away from Planet 9 to not be significantly affected. We therefore omit a more detailed presentation in order to avoid repetition of the conclusions.

  6. In this case, the positions of the planets are therefore different to what the initial test particle population experienced. This is not a problem, however, for two reasons: First, the 119 original particles were extracted at different times (i.e., positions of planets) already, but most importantly, the entering of the polar corridor is, to an excellent approximation, independent of the positions of the planets (Batygin and Morbidelli 2017; Li et al. 2018).

  7. We note that this is most likely an underestimate, since from a code framework perspective, we are restricted to analyzing the orbits at the output time steps of 10 ka. We are therefore missing all particles that enter and leave a planet’s influence in between the snapshots.

  8. We find a similar capture rate into the 1:1 resonance for the clones of the prograde particle.

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Acknowledgements

We thank Nathan A. Kaib and a second anonymous reviewer for their valuable comments and suggestions for improving this manuscript. This research has made use of data and/or services provided by the International Astronomical Union’s Minor Planet Center. Simulations in this paper made use of the REBOUND code which is freely available at https://github.com/hannorein/rebound. KB gratefully acknowledges the David and Lucile Packard Foundation and the Alfred P. Sloan Foundation for their generous support.

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Correspondence to Tobias Köhne.

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This article is part of the topical collection on Trans-Neptunian Objects.

Guest Editors: David Nesvorny and Alessandra Celletti.

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Köhne, T., Batygin, K. On the dynamical origins of retrograde Jupiter Trojans and their connection to high-inclination TNOs. Celest Mech Dyn Astr 132, 44 (2020). https://doi.org/10.1007/s10569-020-09985-1

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  • DOI: https://doi.org/10.1007/s10569-020-09985-1

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