Hubble PanCET: An isothermal day-side atmosphere for the bloated gas-giant HAT-P-32Ab
N. Nikolov, D. K. Sing, J. Goyal, G. W. Henry, H. R. Wakeford, T. M., Evans, M. Lopez-Morales, A. Garcia Munoz, L. Ben-Jaffel, J. Sanz-Forcada, G., E. Ballester, T. Kataria, J. K. Barstow, V. Bourrier, L. A. Buchhave, O., Cohen, D. Deming, D. Ehrenreich, H. Knutson, P Lavvas

TL;DR
This study presents a detailed thermal emission spectrum of the hot Jupiter HAT-P-32Ab, revealing an isothermal atmosphere with possible thermal inversion, and discusses implications for atmospheric composition and properties.
Contribution
First to provide a high-precision emission spectrum of HAT-P-32Ab from HST, combined with modeling to characterize its atmospheric temperature profile and composition.
Findings
Spectrum consistent with an isothermal atmosphere at ~2000K
Evidence suggests possible VO emission at WFC3 wavelengths
No detection of the 1.4 micron water feature
Abstract
We present a thermal emission spectrum of the bloated hot Jupiter HAT-P-32Ab from a single eclipse observation made in spatial scan mode with the Wide Field Camera 3 (WFC3) aboard the Hubble Space Telescope (HST). The spectrum covers the wavelength regime from 1.123 to 1.644 microns which is binned into 14 eclipse depths measured to an averaged precision of 104 parts-per million. The spectrum is unaffected by a dilution from the close M-dwarf companion HAT-P-32B, which was fully resolved. We complemented our spectrum with literature results and performed a comparative forward and retrieval analysis with the 1D radiative-convective ATMO model. Assuming solar abundance of the planet atmosphere, we find that the measured spectrum can best be explained by the spectrum of a blackbody isothermal atmosphere with Tp = 1995 +/- 17K, but can equally-well be described by a spectrum with modest…
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