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Title: WARM SPITZER OBSERVATIONS OF THREE HOT EXOPLANETS: XO-4b, HAT-P-6b, AND HAT-P-8b

Journal Article · · Astrophysical Journal
 [1];  [2];  [3];  [4];  [5];  [6];  [7]; ;  [8]; ;  [9];  [10]; ;  [11]
  1. Department of Astronomy and Astrophysics, The Pennsylvania State University, University Park, PA 16802 (United States)
  2. Planetary Systems Laboratory, NASA's Goddard Space Flight Center, Greenbelt, MD 20771 (United States)
  3. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125 (United States)
  4. Department of Astrophysical Sciences, Princeton University, Princeton, NJ 05844 (United States)
  5. Department of Physics and Mathematics, University of Monterrey, Monterrey (Mexico)
  6. Department of Physics and Astronomy, Northwestern University, Evanston, IL 60208 (United States)
  7. Department of Astronomy, University of Washington, Box 351580, Seattle, WA 98195 (United States)
  8. Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138 (United States)
  9. Department of Astronomy and Astrophysics, University of California at Santa Cruz, Santa Cruz, CA 95064 (United States)
  10. Department of Physics, Principia College, Elsah, IL 62028 (United States)
  11. Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721 (United States)

We analyze Warm Spitzer/Infrared Array Camera observations of the secondary eclipses of three planets, XO-4b, HAT-P-6b, and HAT-P-8b. We measure secondary eclipse amplitudes at 3.6 {mu}m and 4.5 {mu}m for each target. XO-4b exhibits a stronger eclipse depth at 4.5 {mu}m than at 3.6 {mu}m, which is consistent with the presence of a temperature inversion. HAT-P-8b shows a stronger eclipse amplitude at 3.6 {mu}m and is best described by models without a temperature inversion. The eclipse depths of HAT-P-6b can be fitted with models with a small or no temperature inversion. We consider our results in the context of a postulated relationship between stellar activity and temperature inversion and a relationship between irradiation level and planet dayside temperature, as discussed by Knutson et al. and Cowan and Agol, respectively. Our results are consistent with these hypotheses, but do not significantly strengthen them. To measure accurate secondary eclipse central phases, we require accurate ephemerides. We obtain primary transit observations and supplement them with publicly available observations to update the orbital ephemerides of the three planets. Based on the secondary eclipse timing, we set upper boundaries for ecos ({omega}) for HAT-P-6b, HAT-P-8b, and XO-4b and find that the values are consistent with circular orbits.

OSTI ID:
22011762
Journal Information:
Astrophysical Journal, Vol. 746, Issue 1; Other Information: Country of input: International Atomic Energy Agency (IAEA); ISSN 0004-637X
Country of Publication:
United States
Language:
English

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