K2 and Spitzer phase curves of the rocky ultra-short-period planet K2-141 b hint at a tenuous rock vapor atmosphere
Authors/Creators
- 1. Max-Planck-Institut für Astronomie, Königstuhl 17, D-69117 Heidelberg, Germany
- 2. Leiden Observatory, Leiden University, Niels Bohrweg 2, 2333CA Leiden, The Netherlands
- 3. Centre for Research in Earth and Space Sciences, York University, 4700 Keele St, Toronto, ON M3J 1P3, Canada
- 4. SRON Netherlands Institute for Space Research, Niels Bohrweg 4, 2333 CA Leiden, the Netherlands
- 5. Department of Earth & Planetary Sciences, McGill University, 3450 rue University, Montréal, QC H3A 0E8, Canada
- 6. Department of Physics, Oxford University, Parks Rd, Oxford, OX1 3PJ, UK
- 7. Department of Physics, McGill University, 3600 University St, Montr\'eal, QC H3A 2T8, Canada
- 8. Department of Physics, University of Warwick, Coventry, CV4 7AL, UK
- 9. Eureka Scientific Inc, Oakland, CA 94602
- 10. Dipartimento di Fisica e Astronomia "Galileo Galilei", Università degli Studi di Padova, Vicolo dell'Osservatorio 3, 35122 Padova, Italy
- 11. Johns Hopkins APL, 11100 Johns Hopkins Rd, Laurel, MD 20723, USA
Description
K2-141 b is a transiting, small (1.5 Re) ultra-short-period (USP) planet discovered by the Kepler space telescope orbiting a K-dwarf host star every 6.7 h. The planet’s high surface temperature of more than 2000 K makes it an excellent target for thermal emission observations. Here we present 65 h of continuous photometric observations of K2-141 b collected with Spitzer’s Infrared Array Camera (IRAC) Channel 2 at 4.5 µm spanning ten full orbits of the planet. We measured an infrared eclipse depth of 143 +/- 39 ppm and a peak to trough amplitude variation of 121 +/- 43 ppm. The best fit model to the Spitzer data shows no significant thermal hotspot offset, in contrast to the previously observed offset for the well-studied USP planet 55 Cnc e. We also jointly analyzed the new Spitzer observations with the photometry collected by Kepler during two separate K2 campaigns. We modeled the planetary emission with a range of toy models that include a reflective and a thermal contribution. With a two-temperature model, we measured a dayside temperature of 2049 +/- 361 K and a night-side temperature that is consistent with zero (Tp,n < 1712 K at 2σ). Models with a steep dayside temperature gradient provide a better fit to the data than a uniform dayside temperature (∆BIC = 22.2). We also found evidence for a nonzero geometric albedo of Ag = 0.28 +/- 0.07. We also compared the data to a physically motivated, pseudo-2D rock vapor model and a 1D turbulent boundary layer model. Both models fit the data well. Notably, we found that the optical eclipse depth can be explained by thermal emission from a hot inversion layer, rather than reflected light. A thermal inversion may also be responsible for the deep optical eclipse observed for another USP, Kepler-10 b. Finally, we significantly improved the ephemerides for K2-141 b and c, which will facilitate further follow-up observations of this interesting system with state-of-the-art observatories such as JWST.
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