Chemical Equilibrium Abundances in Brown Dwarf and Extrasolar Giant Planet Atmospheres

1999 ◽  
Vol 512 (2) ◽  
pp. 843-863 ◽  
Author(s):  
Adam Burrows ◽  
C. M. Sharp
2004 ◽  
Vol 202 ◽  
pp. 269-276
Author(s):  
Mark S. Marley ◽  
Andrew S. Ackerman

Clouds and hazes are important throughout our solar system and in the atmospheres of brown dwarfs and extrasolar giant planets. Among the brown dwarfs, clouds control the colors and spectra of the L-dwarfs; the disappearance of clouds helps herald the arrival of the T-dwarfs. The structure and composition of clouds will be among the first remote-sensing results from the direct detection of extrasolar giant planets.


2008 ◽  
Vol 390 (3) ◽  
pp. 1258-1266 ◽  
Author(s):  
J. R. Barnes ◽  
Travis S. Barman ◽  
H. R. A. Jones ◽  
C. J. Leigh ◽  
A. Collier Cameron ◽  
...  

2018 ◽  
Vol 155 (5) ◽  
pp. 219 ◽  
Author(s):  
Y. K. Jung ◽  
A. Udalski ◽  
A. Gould ◽  
Y.-H. Ryu ◽  
J. C. Yee ◽  
...  

2010 ◽  
Vol 6 (S276) ◽  
pp. 495-496 ◽  
Author(s):  
Leonardo A. Almeida ◽  
Francisco Jablonski

AbstractQS Vir is an eclipsing cataclysmic variable with 3.618 hrs orbital period. This system has the interesting characteristics that it does not show mass transfer between the components through the L1 Lagrangian point and shows a complex orbital period variation history. Qian et al. (2010) associated the orbital period variations to the presence of a giant planet in the system plus angular momentum loss via magnetic braking. Parsons et al. (2010) obtained new eclipse timings and observed that the orbital period variations associated to a hypothetical giant planet disagree with their measurements and concluded that the decrease in orbital period is part of a cyclic variation with period ~16 yrs. In this work, we present 28 new eclipse timings of QS Vir and suggest that the orbital period variations can be explained by a model with two circumbinary bodies. The best fitting gives the lower limit to the masses M1 sin(i) ~ 0.0086 M⊙ and M2 sin(i) ~ 0.054 M⊙; orbital periods P1 ~ 14.4 yrs and P2 ~ 16.99 yrs, and eccentricities e1 ~ 0.62 and e2~0.92 for the two external bodies. Under the assumption of coplanarity among the two external bodies and the inner binary, we obtain a giant planet with ~0.009 M⊙ and a brown dwarf with ~ 0.056 M⊙ around the eclipsing binary QS Vir.


2018 ◽  
Vol 614 ◽  
pp. A16 ◽  
Author(s):  
A. Cheetham ◽  
D. Ségransan ◽  
S. Peretti ◽  
J.-B. Delisle ◽  
J. Hagelberg ◽  
...  

Using high-contrast imaging with the SPHERE instrument at the Very Large Telescope (VLT), we report the first images of a cold brown dwarf companion to the exoplanet host star HD 4113A. The brown dwarf HD 4113C is part of a complex dynamical system consisting of a giant planet, a stellar host, and a known wide M-dwarf companion. Its separation of 535 ± 3 mas and H-band contrast of 13.35 ± 0.10 mag correspond to a projected separation of 22 AU and an isochronal mass estimate of 36 ± 5 MJ based on COND models. The companion shows strong methane absorption, and through fitting an atmosphere model, we estimate a surface gravity of logg = 5 and an effective temperature of ~500–600 K. A comparison of its spectrum with observed T dwarfs indicates a late-T spectral type, with a T9 object providing the best match. By combining the observed astrometry from the imaging data with 27 years of radial velocities, we use orbital fitting to constrain its orbital and physical parameters, as well as update those of the planet HD 4113A b, discovered by previous radial velocity measurements. The data suggest a dynamical mass of 66−4+5 MJ and moderate eccentricity of 0.44−0.07+0.08 for the brown dwarf. This mass estimate appears to contradict the isochronal estimate and that of objects with similar temperatures, which may be caused by the newly detected object being an unresolved binary brown dwarf system or the presence of an additional object in the system. Through dynamical simulations, we show that the planet may undergo strong Lidov-Kozai cycles, raising the possibility that it formed on a quasi-circular orbit and gained its currently observed high eccentricity (e ~ 0.9) through interactions with the brown dwarf. Follow-up observations combining radial velocities, direct imaging, and Gaia astrometry will be crucial to precisely constrain the dynamical mass of the brown dwarf and allow for an in-depth comparison with evolutionary and atmosphere models.


2012 ◽  
Vol 8 (S293) ◽  
pp. 229-234
Author(s):  
Jade C. Carter-Bond ◽  
David P. O'Brien ◽  
Sean N. Raymond

AbstractA diverse range of terrestrial planet compositions is believed to exist within known extrasolar planetary systems, ranging from those that are relatively Earth-like to those that are highly unusual, dominated by species such as refractory elements (Al and Ca) or C (as pure C, TiC and SiC)(Bond et al. 2010b). However, all prior simulations have ignored the impact that giant planet migration during planetary accretion may have on the final terrestrial planetary composition. Here, we combined chemical equilibrium models of the disk around five known planetary host stars (Solar, HD4203, HD19994, HD213240 and Gl777) with dynamical models of terrestrial planet formation incorporating various degrees of giant planet migration. Giant planet migration is found to drastically impact terrestrial planet composition by 1) increasing the amount of Mg-silicate species present in the final body; and 2) dramatically increasing the efficiency and amount of water delivered to the terrestrial bodies during their formation process.


2001 ◽  
Vol 560 (1) ◽  
pp. 413-419 ◽  
Author(s):  
W. B. Hubbard ◽  
J. J. Fortney ◽  
J. I. Lunine ◽  
A. Burrows ◽  
D. Sudarsky ◽  
...  

2004 ◽  
Vol 425 (2) ◽  
pp. L29-L32 ◽  
Author(s):  
G. Chauvin ◽  
A.-M. Lagrange ◽  
C. Dumas ◽  
B. Zuckerman ◽  
D. Mouillet ◽  
...  
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