An Atmosphere on the Ultra-Short Period super-Earth HD 3167 b
Brandon Park Coy, Qiao Xue, Megan Weiner Mansfield, Jason D. Eastman, Anjali A.A. Piette, Tyler Fairnington, Cole Smith, Michael Zhang, Eliza M.R. Kempton, Jacob L. Bean, Xuan Ji, Peter Gao, Jegug Ih, Daniel D.B. Koll, Rafael Luque, Jaume Orell-Miquel, Edwin S. Kite

TL;DR
This study presents JWST observations of the ultra-short period super-Earth HD 3167 b, providing evidence for an atmosphere that influences its thermal emission and refining its planetary parameters.
Contribution
First direct detection of atmospheric effects on an ultra-short period super-Earth using JWST, bridging the gap in understanding atmospheric presence at high instellation flux.
Findings
Measured eclipse depth indicates a cooling atmosphere on HD 3167 b.
The planet's dayside temperature suggests reflection and heat redistribution by an atmosphere.
Refined planetary parameters, confirming atmospheric presence on the least irradiated USP super-Earth.
Abstract
'Lava worlds'-Earth-sized planets hot enough (Teq >~ 1100 K) to melt their dayside silicate surfaces-have emerged as promising candidates for atmospheric detection and characterization. Thermal emission observations show an apparent dichotomy: the hottest lava worlds have colder daysides than the temperature of a maximally emitting bare rock, indicating the likely presence of thick and/or reflective atmospheres while the coldest ones do not. However, where in instellation flux this potential bifurcation occurs is uncertain. We present a JWST MIRI LRS eclipse of the ultra-short period (USP) lava world HD 3167 b (Teq = 1786 K, R = 1.6 Rearth, P = 0.96 d) that helps bridge this gap. We measure the white light eclipse depth to be 38 +/- 11 ppm, more than 5 sigma lower than the expected eclipse depth of a dark, maximally hot bare rock. We use this to derive a dayside brightness temperature…
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