Dynamically hot Super-Earths from outer giant planet scattering
Chelsea X. Huang, Cristobal Petrovich, Emily Deibert

TL;DR
This paper uses N-body simulations to show that outer giant planet scattering can dynamically heat inner super-Earth systems, leading to hot, eccentric, and inclined single-transiting planets, explaining several Kepler observations.
Contribution
It introduces a model where outer giant planet scattering explains the hot, eccentric, and inclined nature of some single-transiting super-Earths observed by Kepler.
Findings
Outer giant planets reduce inner system multiplicity.
Surviving inner planets can have high eccentricities and inclinations.
Model explains Kepler's eccentricity and obliquity observations.
Abstract
The hundreds of multiple planetary systems discovered by the \textit{Kepler} mission are typically observed to reside in close-in ( AU), low-eccentricity, and low-inclination orbits. We run N-body experiments to study the effect that unstable outer ( AU) giant planets, whose end orbital configurations resemble those in the Radial Velocity population, have on these close-in multiple super-Earth systems. Our experiments show that the giant planets greatly reduce the multiplicity of the inner super-Earths and the surviving population can have large eccentricities () and inclinations () at levels that anti-correlate with multiplicity. Consequently, this model predicts the existence of a population of dynamically hot single-transiting planets with typical eccentricities and inclinations %in the ranges of and $\sim…
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