SPITZER OBSERVATIONS OF THE THERMAL EMISSION FROM WASP-43b

被引:76
作者
Blecic, Jasmina [1 ]
Harrington, Joseph [1 ,2 ]
Madhusudhan, Nikku [3 ,4 ]
Stevenson, Kevin B. [1 ]
Hardy, Ryan A. [1 ]
Cubillos, Patricio E. [1 ,2 ]
Hardin, Matthew [1 ]
Bowman, Oliver [1 ]
Nymeyer, Sarah [1 ]
Anderson, David R. [5 ]
Hellier, Coel [5 ]
Smith, Alexis M. S. [5 ]
Cameron, Andrew Collier [6 ]
机构
[1] Univ Cent Florida, Dept Phys, Planetary Sci Grp, Orlando, FL 32816 USA
[2] Max Planck Inst Astron, D-69117 Heidelberg, Germany
[3] Yale Univ, Dept Phys, New Haven, CT 06511 USA
[4] Yale Univ, Dept Astron, New Haven, CT 06511 USA
[5] Keele Univ, Astrophys Grp, Keele ST5 5BG, Staffs, England
[6] Univ St Andrews, Sch Phys & Astron, SUPA, St Andrews KY16 9SS, Fife, Scotland
关键词
eclipses; planets and satellites: atmospheres; planets and satellites: individual (WASP-43b); techniques: photometric; COLLISION-INDUCED ABSORPTION; HUBBLE-SPACE-TELESCOPE; INFRARED ARRAY CAMERA; SUPER-EARTH GJ1214B; PLANET HD 189733B; EXOPLANET GJ 436B; LOW-MASS STARS; 8; MU-M; HOT JUPITERS; WARM SPITZER;
D O I
10.1088/0004-637X/781/2/116
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
WASP-43b is one of the closest-orbiting hot Jupiters, with a semimajor axis of a = 0.01526 +/- 0.00018 AU and a period of only 0.81 days. However, it orbits one of the coolest stars with a hot Jupiter (T-* = 4520 +/- 120 K), giving the planet a modest equilibrium temperature of T-eq = 1440 +/- 40 K, assuming zero Bond albedo and uniform planetary energy redistribution. The eclipse depths and brightness temperatures from our jointly fit model are 0.347% +/- 0.013% and 1670 +/- 23 K at 3.6 mu m and 0.382% +/- 0.015% and 1514 +/- 25 K at 4.5 mu m. The eclipse timings improved the estimate of the orbital period, P, by a factor of three (P = 0.81347436 +/- 1.4 x 10(-7) days) and put an upper limit on the eccentricity (e = 0.010(-0.007)(+0.010)). We use our Spitzer eclipse depths along with four previously reported ground-based photometric observations in the near- infrared to constrain the atmospheric properties of WASP- 43b. The data rule out a strong thermal inversion in the dayside atmosphere of WASP- 43b. Model atmospheres with no thermal inversions and fiducial oxygen-rich compositions are able to explain all the available data. However, a wide range of metallicities and C/ O ratios can explain the data. The data suggest low day-night energy redistribution in the planet, consistent with previous studies, with a nominal upper limit of about 35% for the fraction of energy incident on the dayside that is redistributed to the nightside.
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页数:11
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