A record of the final phase of giant planet migration fossilized in the asteroid belt's orbital structure
Matthew S. Clement, Alessandro Morbidelli, Sean N. Raymond, Nathan A., Kaib

TL;DR
This paper demonstrates how the final phase of giant planet migration shaped the asteroid belt's orbital structure, especially its inclination distribution, by using numerical simulations aligned with the Nice Model.
Contribution
It reveals the role of the last phase of giant planet migration in sculpting the asteroid belt's inclination distribution, improving previous models.
Findings
The final migration phase influences asteroid inclination distribution.
Slowing and speeding of Saturn's precession affects asteroid excitation.
Simulations match observed asteroid orbital structures more closely.
Abstract
The asteroid belt is characterized by an extreme low total mass of material on dynamically excited orbits. The Nice Model explains many peculiar qualities of the solar system, including the belt's excited state, by invoking an orbital instability between the outer planets. However, previous studies of the Nice Model's effect on the belt's structure struggle to reproduce the innermost asteroids' orbital inclination distribution. Here, we show how the final phase of giant planet migration sculpts the asteroid belt, in particular its inclination distribution. As interactions with leftover planetesimals cause Saturn to move away from Jupiter, its rate of orbital precession slows as the two planets' mutual interactions weaken. When the planets approach their modern separation, where Jupiter completes just short of five orbits for every two of Saturn's, Jupiter's eccentric forcing on Saturn…
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