2019A&A...622A.121O


Query : 2019A&A...622A.121O

2019A&A...622A.121O - Astronomy and Astrophysics, volume 622A121-121 (2019/2-1)

ARCiS framework for exoplanet atmospheres. The cloud transport model.

ORMEL C.W. and MIN M.

Abstract (from CDS):


Context. Understanding of clouds is instrumental in interpreting current and future spectroscopic observations of exoplanets. Modeling clouds consistently is complex, since it involves many facets of chemistry, nucleation theory, condensation physics, coagulation, and particle transport.
Aims. We aim to develop a simple physical model for cloud formation and transport, efficient and versatile enough that it can be used, in modular fashion for parameter optimization searches of exoplanet atmosphere spectra. d(Σn)/dt on the planet's observational characteristics.
Methods. The transport equations are formulated in 1D, accounting for sedimentation and diffusion. The grain size is obtained through a moment method. For simplicity, only one cloud species is considered and the nucleation rate is parametrized. From the resulting physical profiles we simulate transmission spectra covering the visual to mid-IR wavelength range.
Results. We apply our models toward KCl clouds in the atmosphere of GJ1214 b and toward MgSiO3 clouds of a canonical hot-Jupiter. We find that larger K increases the thickness of the cloud, pushing the τ=1 surface to a lower pressure layer higher in the atmosphere. A larger nucleation rate also increases the cloud thickness while it suppresses the grain size. Coagulation is most important at high d(Σn)/dt low K. We find that the investigated combinations of K and d(Σn)/dt greatly affect the transmission spectra in terms of the slope at near-IR wavelength (a proxy for grain size), the molecular features seen at approximately µm (which disappear for thick clouds, high in the atmosphere), and the 10µm silicate feature, which becomes prominent for small grains high in the atmosphere.
Conclusions. Clouds have a major impact on the atmospheric characteristics of hot-Jupiters, and models as those presented here are necessary to reveal the underlying properties of exoplanet atmospheres. The result of our hybrid approach - aimed to provide a good balance between physical consistency and computational efficiency - is ideal toward interpreting (future) spectroscopic observations of exoplanets.

Abstract Copyright: © ESO 2019

Journal keyword(s): methods: numerical - planets and satellites: atmospheres - planets and satellites: composition

Simbad objects: 1

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Number of rows : 1
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 NAME G 139-21b Pl 17 15 18.9339850845 +04 57 50.066612336           ~ 845 1

Query : 2019A&A...622A.121O

Basic data :
NAME G 139-21b -- Extra-solar Planet
Other object types:
otypes_help
Pl (), Pl? (), * (GJ)
ICRS coord. (ep=J2000) :
17 15 18.9339850845 +04 57 50.066612336 (Optical) [ 0.0459 0.0382 90 ] A 2020yCat.1350....0G
FK4 coord. (ep=B1950 eq=1950) :
17 12 48.9435356455 +05 01 47.135421918 [ 0.0459 0.0382 90 ]
Gal coord. (ep=J2000) :
026.1640350986908 +23.6107452581176 [ 0.0459 0.0382 90 ]
Proper motions mas/yr :
580.202 -749.713 [0.059 0.047 90] A 2020yCat.1350....0G
Parallaxes (mas):
68.2986 [0.0652] A 2020yCat.1350....0G
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GJ 1214 b NAME LHS 3275b NAME G 139-21b NAME-IAU Enaiposha

References (845 between 1850 and 2026) (Total 845)
Simbad bibliographic survey began in 1850 for stars (at least bright stars) and in 1983 for all other objects (outside the solar system).
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