A SEMI-ANALYTICAL MODEL OF VISIBLE-WAVELENGTH PHASE CURVES OF EXOPLANETS AND APPLICATIONS TO KEPLER-7 B AND KEPLER-10 B

被引:57
|
作者
Hu, Renyu [1 ,2 ]
Demory, Brice-Olivier [3 ]
Seager, Sara [4 ,5 ]
Lewis, Nikole [4 ]
Showman, Adam P. [6 ]
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[2] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[3] Univ Cambridge, Cavendish Lab, Astrophys Grp, Cambridge CB3 0HE, England
[4] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
[5] MIT, Dept Phys, Cambridge, MA 02139 USA
[6] Univ Arizona, Dept Planetary Sci, Tucson, AZ 85721 USA
来源
ASTROPHYSICAL JOURNAL | 2015年 / 802卷 / 01期
关键词
atmospheric effects; planets and satellites: individual (Kepler-7 b; Kepler-10; b); radiative transfer; techniques: photometric; TIDALLY LOCKED EXOPLANETS; ATMOSPHERIC CIRCULATION; HOT JUPITERS; THEORETICAL SPECTRA; LIGHT CURVES; HEAT REDISTRIBUTION; EXTRASOLAR PLANETS; TRANSITING PLANETS; POLARIZATION; PHOTOCHEMISTRY;
D O I
10.1088/0004-637X/802/1/51
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Kepler has detected numerous exoplanet transits by measuring stellar light in a single visible-wavelength band. In addition to detection, the precise photometry provides phase curves of exoplanets, which can be used to study the dynamic processes on these planets. However, the interpretation of these observations can be complicated by the fact that visible-wavelength phase curves can represent both thermal emission and scattering from the planets. Here we present a semi-analytical model framework that can be applied to study Kepler and future visible-wavelength phase curve observations of exoplanets. The model efficiently computes reflection and thermal emission components for both rocky and gaseous planets, considering both homogeneous and inhomogeneous surfaces or atmospheres. We analyze the phase curves of the gaseous planet Kepler-7 b and the rocky planet Kepler-10 b using the model. In general, we find that a hot exoplanet's visible-wavelength phase curve having a significant phase offset can usually be explained by two classes of solutions: one class requires a thermal hot spot shifted to one side of the substellar point, and the other class requires reflective clouds concentrated on the same side of the substellar point. Particularly for Kepler-7 b, reflective clouds located on the west side of the substellar point can best explain its phase curve. The reflectivity of the clear part of the atmosphere should be less than 7% and that of the cloudy part should be greater than 80%, and the cloud boundary should be located at 11 degrees +/- 3 degrees to the west of the substellar point. We suggest single-band photometry surveys could yield valuable information on exoplanet atmospheres and surfaces.
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页数:15
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