Abstract
The eccentric orbits of the known extrasolar giant planets provide evidence that most planet-forming environments undergo violent dynamical instabilities. Here, we numerically simulate the impact of giant planet instabilities on planetary systems as a whole. We find that populations of inner rocky and outer icy bodies are both shaped by the giant planet dynamics and are naturally correlated. Strong instabilities - those with very eccentric surviving giant planets - completely clear out their inner and outer regions. In contrast, systems with stable or low-mass giant planets form terrestrial planets in their inner regions and outer icy bodies produce dust that is observable as debris disks at mid-infrared wavelengths. Fifteen to twenty percent of old stars are observed to have bright debris disks (at λ ∼ 70μm) and we predict that these signpost dynamically calm environments that should contain terrestrial planets. © International Astronomical Union 2011.
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Raymond, S. N., Armitage, P. J., Moro-Martín, A., Booth, M., Wyatt, M. C., Armstrong, J. C., … Selsis, F. (2010). The debris disk - Terrestrial planet connection. In Proceedings of the International Astronomical Union (Vol. 6, pp. 82–88). https://doi.org/10.1017/S1743921311019983
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