The Astronomical Journal (Jan 2023)

Keck Planet Imager and Characterizer Emission Spectroscopy of WASP-33b

  • Luke Finnerty,
  • Tobias Schofield,
  • Ben Sappey,
  • Jerry W. Xuan,
  • Jean-Baptiste Ruffio,
  • Jason J. Wang,
  • Jacques-Robert Delorme,
  • Geoffrey A. Blake,
  • Cam Buzard,
  • Michael P. Fitzgerald,
  • Ashley Baker,
  • Randall Bartos,
  • Charlotte Z. Bond,
  • Benjamin Calvin,
  • Sylvain Cetre,
  • Greg Doppmann,
  • Daniel Echeverri,
  • Nemanja Jovanovic,
  • Joshua Liberman,
  • Ronald A. López,
  • Emily C. Martin,
  • Dimitri Mawet,
  • Evan Morris,
  • Jacklyn Pezzato,
  • Caprice L. Phillips,
  • Sam Ragland,
  • Andrew Skemer,
  • Taylor Venenciano,
  • J. Kent Wallace,
  • Nicole L. Wallack,
  • Ji Wang,
  • Peter Wizinowich

DOI
https://doi.org/10.3847/1538-3881/acda91
Journal volume & issue
Vol. 166, no. 1
p. 31

Abstract

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We present Keck Planet Imager and Characterizer (KPIC) high-resolution ( R ∼35,000) K -band thermal emission spectroscopy of the ultrahot Jupiter WASP-33b. The use of KPIC’s single-mode fibers greatly improves both blaze and line-spread stabilities relative to slit spectrographs, enhancing the cross-correlation detection strength. We retrieve the dayside emission spectrum with a nested-sampling pipeline, which fits for orbital parameters, the atmospheric pressure–temperature profile, and the molecular abundances. We strongly detect the thermally inverted dayside and measure mass-mixing ratios for CO ( ${\mathrm{logCO}}_{\mathrm{MMR}}=-{1.1}_{-0.6}^{+0.4}$ ), H _2 O ( ${\mathrm{logH}}_{2}{{\rm{O}}}_{\mathrm{MMR}}\,=-{4.1}_{-0.9}^{+0.7}$ ), and OH ( ${\mathrm{logOH}}_{\mathrm{MMR}}=-{2.1}_{-1.1}^{+0.5}$ ), suggesting near-complete dayside photodissociation of H _2 O. The retrieved abundances suggest a carbon- and possibly metal-enriched atmosphere, with a gas-phase C/O ratio of ${0.8}_{-0.2}^{+0.1}$ , consistent with the accretion of high-metallicity gas near the CO _2 snow line and post-disk migration or with accretion between the soot and H _2 O snow lines. We also find tentative evidence for ^12 CO/ ^13 CO ∼ 50, consistent with values expected in protoplanetary disks, as well as tentative evidence for a metal-enriched atmosphere (2–15 × solar). These observations demonstrate KPIC’s ability to characterize close-in planets and the utility of KPIC’s improved instrumental stability for cross-correlation techniques.

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