ArXiv TLDR

Confirmation of Fe I on MASCARA-5 b's Dayside Observed With EXPRES

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2605.00154

James T. Sikora, Joe Llama, Rachael M. Roettenbacher, Elisabeth M. Brann, Jean-Michel Désert + 3 more

astro-ph.EP

TLDR

New EXPRES observations confirm iron (Fe I) on the dayside of ultra-hot Jupiter MASCARA-5 b, revealing a strong thermal inversion and potential winds.

Key contributions

  • Confirmed Fe I on MASCARA-5 b's dayside with 5.5σ significance using EXPRES.
  • Verified the planet's atmosphere has a strong thermal inversion (2000K to 4500K).
  • Observed a blueshift in the pre-eclipse signal, suggesting high-altitude winds.
  • No detection of Fe II or Cr I was found in the atmosphere.

Why it matters

Characterizing ultra-hot Jupiter atmospheres helps us understand extreme planetary environments. This study provides crucial observational evidence for atmospheric chemistry, thermal structure, and dynamics, informing future exoplanet models.

Original Abstract

MASCARA-5~b/TOI-1431~b is an ultra-hot Jupiter \citep[$P_{\rm orb}=2.650237\pm0.000003\,{\rm d}$, $T_{\rm eq}=2370\pm70\,{\rm K}$, $M_{\rm p}=3.12\pm0.18\,M_{\rm Jup}$, $R_{\rm p}=1.49\pm0.05\,R_{\rm Jup}$;][]{addison2021} orbiting a bright Am star ($V=8.0\,{\rm mag}$). Recent time-series observations obtained with PEPSI@LBT during the planet's post-eclipse phases have revealed Fe~{\sc i} emission lines indicative of a thermally inverted atmosphere. These observations demonstrate that MASCARA-5~b is well-suited to atmospheric characterization via emission spectroscopy, thereby motivating further follow-up observations covering additional orbital phases to constrain the planet's atmospheric chemistry, thermal structure, and dynamics. Here we present pre-eclipse time-series observations obtained with the high-resolution optical spectrograph EXPRES@LDT. Our analysis confirms the previous detection of gas-phase Fe~{\sc i} on MASCARA-5~b's dayside (with a $5.5σ$ significance obtained from two nights of observations) and the fact that the thermal profile is inverted with lower and upper temperatures $\sim2000\,{\rm K}$ and $\sim4500\,{\rm K}$, respectively. A search for Fe~{\sc ii} and Cr~{\sc i} did not yield any plausible detections. We also find that the pre-eclipse signal exhibits a non-negligible blueshift of $-3.2\pm1.4\,{\rm km/s}$ potentially caused by winds.

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