Wasp-17b versus other hot-Jupiters being surveyed with HST: A clear versus dusty/hazy atmospheres
Abstract
A large HST optical and near-IR spectral survey of eight hot-Jupiter exoplanets is being carried out (D. Sing, PI) in which we are studying planets spanning a large temperature regime (1000-3000 K). Together with previous HST observations, this program is showing hot Jupiters with lower atmospheres where the optical and near-IR transit signatures are dominated by, or have a significant contribution from, scattering by aerosols. This is the well-known case for the relatively cooler HD 189733b on which fine silicate grains may have been detected (Pont et al. 2008, 2013; Lecavelier et al. 2008; Sing et al. 2011; Evans et al. 2013), the more recent case of the hotter Hat-P-1b (Wakeford et al. 2013; Nikolov et al. 2013), and the surprising case of the very-hot-Jupiter Wasp-12b on which fine-grains of corundum may have been detected (Sing et al. 2013). Evidence for aerosols has also been found with Kepler for Kepler-7b (Demory et al. 2013).
Under this large HST survey, we have recently observed transits of Wasp-17b in the optical with HST/STIS, and we are combining these data with archival HST/WFC3 near-IR (1.09-1.69 microns) transit data and with Spitzer/IRAC 4.5 and 8 um transit photometry (Ballester et al. 2014). Wasp-17b presents an interesting case of the most highly inflated hot Jupiter (0.49 MJup, 1.99 RJup) known to date that is also on a retrograde orbit (at 0.0515 AU around a hot F6V star) indicating a violent history for the system (Anderson et al. 2010). The average dayside temperature for the planet is 1580-1880 K (Anderson et al. 2011). In contrast to the above cases of dusty/hazy atmospheres, our preliminary results show a clear atmosphere on Wasp-17b. The planet presents the best case so far of a hot Jupiter that is consistent with a cloud-free atmosphere given that the optical radius is much smaller than the near-IR radius (i.e., scattering by dust or haze is not obscuring the expected transit signatures of a clear lower atmosphere). Water absorption is detected. We are also finding a stronger Na I line-core absorption that predicted by models (which may evidence sodium over-abundance at high altitudes), while at the same time we find no evidence for K I absorption. This alkali behavior is not unique to Wasp-17b, since similar results have been found with HST for HD 189733b (Huitson et al. 2012) and Hat-P-1b (Nikolov et al. 2013). The work is in progress, and more detailed results will be presented and compared with other observations of this planet.- Publication:
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Search for Life Beyond the Solar System. Exoplanets, Biosignatures & Instruments
- Pub Date:
- March 2014
- Bibcode:
- 2014ebi..confP3.48B