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Gemini/GMOS Transmission Spectroscopy of the Grazing Planet Candidate WD 1856+534 b

  • Siyi Xu*
  • , Hannah Diamond-Lowe
  • , Ryan J. MacDonald
  • , Andrew Vanderburg
  • , Simon Blouin
  • , P. Dufour
  • , Peter Gao
  • , Laura Kreidberg
  • , S. K. Leggett
  • , Andrew W. Mann
  • , Caroline V. Morley
  • , Andrew W. Stephens
  • , Christopher E. O’Connor
  • , Pa Chia Thao
  • , Nikole K. Lewis
  • *Corresponding author for this work
    • Gemini Observatory
    • Cornell University
    • Massachusetts Institute of Technology
    • Los Alamos National Laboratory
    • Université de Montréal
    • University of California at Santa Cruz
    • Max Planck Institute for Astronomy
    • University of North Carolina at Chapel Hill
    • University of Texas at Austin

    Research output: Contribution to journal › Journal article › Research › peer-review

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    Abstract

    WD1856+534 b is a Jupiter-sized, cool giant planet candidate transiting the white dwarf WD1856+534. Here, we report an optical transmission spectrum of WD1856+534 b obtained from ten transits using the Gemini Multi- Object Spectrograph. This system is challenging to observe due to the faintness of the host star and the short transit duration. Nevertheless, our phase-folded white light curve reached a precision of 0.12%. WD1856+534 b provides a unique transit configuration compared to other known exoplanets: the planet is 8× larger than its star and occults over half of the stellar disk during mid-transit. Consequently, many standard modeling assumptions do not hold. We introduce the concept of a “limb darkening corrected, time-averaged transmission spectrum” and propose that this is more suitable than (Rp,λ,l Rs)2 for comparisons to atmospheric models for planets with grazing transits. We also present a modified radiative transfer prescription. Though the transmission spectrum shows no prominent absorption features, it is sufficiently precise to constrain the mass of WD1856+534 b to be >0.84 MJ (to 2σ confidence), assuming a clear atmosphere and a Jovian  composition. High-altitude cloud decks can allow lower masses. WD1856+534 b could have formed either as a result of common envelope evolution or migration under the Kozai–Lidov mechanism. Further studies of WD1856+534 b, alongside new dedicated searches for substellar objects around white dwarfs, will shed further light on the mysteries of post-main-sequence planetary systems.
    Original languageEnglish
    Article number296
    JournalAstronomical Journal
    Volume162
    Issue number6
    Number of pages15
    ISSN0004-6256
    DOIs
    Publication statusPublished - 2021

    Keywords

    • Exoplanet atmospheres
    • White dwarf stars
    • Extrasolar gaseous planets
    • Brown dwarfs

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