tidal deformation
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Author(s):  
S. C. C. Barros ◽  
B. Akinsanmi ◽  
G. Boué ◽  
A. M. S. Smith ◽  
J. Laskar ◽  
...  
Keyword(s):  


Icarus ◽  
2021 ◽  
pp. 114714
Author(s):  
Andrei A. Dmitrovskii ◽  
Amir Khan ◽  
Christian Boehm ◽  
Amirhossein Bagheri ◽  
Martin van Driel




2020 ◽  
Vol 160 (6) ◽  
pp. 272
Author(s):  
Cheng-Gang Qin ◽  
Yu-Jie Tan ◽  
Ceng-Gang Shao


2020 ◽  
Vol 900 (1) ◽  
pp. 49
Author(s):  
N. K. Patra ◽  
Tuhin Malik ◽  
Debashree Sen ◽  
T. K. Jha ◽  
Hiranmaya Mishra




2020 ◽  
Vol 635 ◽  
pp. A117 ◽  
Author(s):  
E. Bolmont ◽  
B.-O. Demory ◽  
S. Blanco-Cuaresma ◽  
E. Agol ◽  
S. L. Grimm ◽  
...  

Transit timing variations (TTVs) can be a very efficient way of constraining masses and eccentricities of multi-planet systems. Recent measurements of the TTVs of TRAPPIST-1 have led to an estimate of the masses of the planets, enabling an estimate of their densities and their water content. A recent TTV analysis using data obtained in the past two years yields a 34 and 13% increase in mass for TRAPPIST-1b and c, respectively. In most studies to date, a Newtonian N-body model is used to fit the masses of the planets, while sometimes general relativity is accounted for. Using the Posidonius N-body code, in this paper we show that in the case of the TRAPPIST-1 system, non-Newtonian effects might also be relevant to correctly model the dynamics of the system and the resulting TTVs. In particular, using standard values of the tidal Love number k2 (accounting for the tidal deformation) and the fluid Love number k2f (accounting for the rotational flattening) leads to differences in the TTVs of TRAPPIST-1b and c that are similar to the differences caused by general relativity. We also show that relaxing the values of tidal Love number k2 and the fluid Love number k2f can lead to TTVs which differ by as much as a few 10 s on a 3−4-yr timescale, which is a potentially observable level. The high values of the Love numbers needed to reach observable levels for the TTVs could be achieved for planets with a liquid ocean, which if detected might then be interpreted as a sign that TRAPPIST-1b and TRAPPIST-1c could have a liquid magma ocean. For TRAPPIST-1 and similar systems the models to fit the TTVs should potentially account for general relativity, for the tidal deformation of the planets, for the rotational deformation of the planets, and to a lesser extent for the rotational deformation of the star, which would add up to 7 × 2 + 1 = 15 additional free parameters in the case of TRAPPIST-1.





2019 ◽  
Vol 100 (4) ◽  
Author(s):  
Bhaskar Biswas ◽  
Rana Nandi ◽  
Prasanta Char ◽  
Sukanta Bose


2019 ◽  
Vol 621 ◽  
pp. A117 ◽  
Author(s):  
B. Akinsanmi ◽  
S. C. C. Barros ◽  
N. C. Santos ◽  
A. C. M. Correia ◽  
P. F. L. Maxted ◽  
...  

Context. Short-period planets are influenced by the extreme tidal forces of their parent stars. These forces deform the planets causing them to attain nonspherical shapes. The nonspherical shapes, modeled here as triaxial ellipsoids, can have an impact on the observed transit light-curves and the parameters derived for these planets. Aims. We investigate the detectability of tidal deformation in short-period planets from their transit light curves and the instrumental precision needed. We also aim to show how detecting planet deformation allows us to obtain an observational estimate of the second fluid Love number from the light curve, which provides valuable information about the internal structure of the planet. Methods. We adopted a model to calculate the shape of a planet due to the external potentials acting on it and used this model to modify the ellc transit tool. We used the modified ellc to generate the transit light curve for a deformed planet. Our model is parameterized by the Love number; therefore, for a given light curve we can derive the value of the Love number that best matches the observations. Results. We simulated the known cases of WASP-103b and WASP-121b which are expected to be highly deformed. Our analyses show that instrumental precision ≤50 ppm min−1 is required to reliably estimate the Love number and detect tidal deformation. This precision can be achieved for WASP-103b in ∼40 transits using the Hubble Space Telescope and in ∼300 transits using the forthcoming CHEOPS instrument. However, fewer transits will be required for short-period planets that may be found around bright stars in the TESS and PLATO survey missions. The unprecedented precisions expected from PLATO and JWST will permit the detection of shape deformation with a single transit observation. However, the effects of instrumental and astrophysical noise must be considered as they can increase the number of transits required to reach the 50 ppm min−1 detection limit. We also show that improper modeling of limb darkening can act to bury signals related to the shape of the planet, thereby leading us to infer sphericity for a deformed planet. Accurate determination of the limb darkening coefficients is therefore required to confirm planet deformation.



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