![]() Padova University |
![]() Physics & Astronomy Dep. |
![]() Asiago Observatory |
![]() Padova Observatory |
Nascimbeni et al. 2011, A&A 527, 85
A promising method to detect Earth-sized exoplanets is the so-called Transit Time Variation analysis (TTV). By monitoring a known transiting planet with high-precision photometry, the central instant T0 of each individual transit can be estimated. The gravitational perturbation of a previously unknown third body, which is not necessarily transiting, can cause a significant variation of the orbital period P (Holman & Murray 2005, Science 307, 1288). The effect is dependent on the mass of the third body, and is greatly increased if the perturber is locked in a low-order mean-motion resonance with the transiting planet (Agol et al. 2005, MNRAS 359, 567), resulting in typical amplitudes of 10-100 s or even more. The TTV technique has been exploited and already gave amazing results on a large number of planetary systems discovered by the Kepler mission, the most representative being Kepler-11 (Lissauer et al. 2011, Nature, 470, 53). The presence of an exomoon, which makes the planet oscillate around the planet-satellite barycenter along its path, may also cause a periodic TDV (Transit Duration Variation; Kipping 2009a, MNRAS, 392, 181) as well as a TTV, which can reach an amplitude of 10-15 s in the case of 1 M_Earth Hill-stable exomoon around a Neptunian transiting planet.