Into the red: an M-band study of the chemistry and rotation of β Pictoris b at high spectral resolution

Author:

Parker Luke T1ORCID,Birkby Jayne L1ORCID,Landman Rico2,Wardenier Joost P34ORCID,Young Mitchell E15ORCID,Vaughan Sophia R1ORCID,van Sluijs Lennart16,Brogi Matteo78,Parmentier Vivien9,Line Michael R10

Affiliation:

1. Astrophysics, University of Oxford , Denys Wilkinson Building, Keble Road, Oxford OX1 3RH , UK

2. Leiden Observatory, Leiden University , Postbus 9513, NL-2300 RA Leiden , the Netherlands

3. Atmospheric, Oceanic, and Planetary Physics, Clarendon Laboratory, University of Oxford , Oxford OX1 3PU , UK

4. Département de Physique, Institut Trottier de Recherche sur les Exoplanètes, Université de Montréal , Montréal, Québec H3T 1J4 , Canada

5. Astrophysics Research Centre, Queen’s University Belfast , Belfast BT7 1NN , UK

6. Department of Astronomy, University of Michigan , 1085 South University Avenue, Ann Arbor, MI 48109 , USA

7. Dipartimento di Fisica, Università degli Studi di Torino , Via Pietro Giuria 1, I-10125 Torino , Italy

8. INAF – Osservatorio Astrofisico di Torino , Via Osservatorio 20, I-10025 Pino Torinese , Italy

9. Université Côte d’Azur, Observatoire de la Côte d’Azur, CNRS , Laboratoire Lagrange, Nice 06304 , France

10. School of Earth & Space Exploration, Arizona State University , Tempe, AZ 85287 , USA

Abstract

ABSTRACT High-resolution cross-correlation spectroscopy (HRCCS) combined with adaptive optics has been enormously successful in advancing our knowledge of exoplanet atmospheres, from chemistry to rotation and atmospheric dynamics. This powerful technique now drives major science cases for ELT instrumentation including METIS/ELT, GMTNIRS/GMT, and MICHI/TMT, targeting biosignatures on rocky planets at 3–5 μm, but remains untested beyond 3.5 μm where the sky thermal background begins to provide the dominant contribution to the noise. We present 3.51–5.21 μm M-band CRIRES+/VLT observations of the archetypal young directly imaged gas giant β Pictoris b, detecting CO absorption at S/N = 6.6 at 4.73 μm and H2O at S/N = 5.7, and thus extending the use of HRCCS into the thermal background noise dominated infrared. Using this novel spectral range to search for more diverse chemistry, we report marginal evidence of SiO at S/N = 4.3, potentially indicative that previously proposed magnesium–silicate clouds in the atmosphere are either patchy, transparent at M-band wavelengths, or possibly absent on the planetary hemisphere observed. The molecular detections are rotationally broadened by the spin of β Pic b, and we infer a planetary rotation velocity of vsin(i) = 22 ± 2 km s−1 from the cross-correlation with the H2O model template, consistent with previous K-band studies. We discuss the observational challenges posed by the thermal background and telluric contamination in the M-band, the custom analysis procedures required to mitigate these issues, and the opportunities to exploit this new infrared window for HRCCS using existing and next-generation instrumentation.

Funder

European Research Council

National Aeronautics and Space Administration

California Institute of Technology

Publisher

Oxford University Press (OUP)

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