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Tidal Evolution of Exoplanets
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Tidal effects arise from differential and inelastic deformation of a planet by a perturbing body. The continuous action of tides modify the rotation of the planet together with its orbit until an equilibrium situation is reached. It is often believed that synchronous motion is the most probable outcome of the tidal evolution process, since synchronous rotation is observed for the majority of the satellites in the Solar System. However, in the 19th century, Schiaparelli also assumed synchronous motion for the rotations of Mercury and Venus, and was later shown to be wrong. Rather, for planets in eccentric orbits synchronous rotation is very unlikely. The rotation period and axial tilt of exoplanets is still unknown, but a large number of planets have been detected close to the parent star and should have evolved to a final equilibrium situation. Therefore, based on the Solar System well studied cases, we can make some predictions for exoplanets. Here we describe in detail the main tidal effects that modify the secular evolution of the spin and the orbit of a planet. We then apply our knowledge acquired from Solar System situations to exoplanet cases. In particular, we will focus on two classes of planets, "Hot-Jupiters" (fluid) and "Super-Earths" (rocky with atmosphere).
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Cited by 2 Pith papers
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TrES-1 b: A Case Study in Detecting Secular Evolution of Exoplanet Orbits
Transit, eclipse and radial velocity data of hot Jupiter TrES-1 b show secular orbital changes, best matched by either apsidal precession requiring an unseen companion or tidal orbital decay at -7.1 ms/yr.
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Investigating Transit Timing Variations in the Ultra-short Period Exoplanet WASP-19b
Transit timing variations of WASP-19b are best explained by apsidal precession with a roughly 18.6-year period, not by an additional planet or by orbital decay.
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