Retrieving wind properties from the ultra-hot dayside of WASP-189 b with CRIRES<sup>+</sup>

Context . The extreme temperature gradients from day- to nightside in the atmospheres of hot Jupiters generate fast winds in the form of equatorial jets or day-to-night flows. Observations of blue-shifted and red-shifted signals in the transmission and dayside spectra of WASP-189 b have sparked discussions about the nature of winds on this planet. Aims . To investigate the structure of winds in the atmosphere of the ultra-hot Jupiter WASP-189 b, we studied its dayside emission spectrum with CRIRES + in the spectral K band. Methods . After removing stellar and telluric lines, we used the cross-correlation method to search for a range of molecules and detected emission signals of CO and Fe. Subsequently, we employed a Bayesian framework to retrieve the atmospheric parameters relating to the temperature–pressure structure and chemistry, and incorporated a numerical model of the line profile influenced by various dynamic effects to determine the wind structure. Results . The cross-correlation signals of CO and Fe showed a velocity offset of ~6 km s −1 , which could be caused by a fast day-tonight wind in the atmosphere of WASP-189 b. The atmospheric retrieval showed that the line profile of the observed spectra is best fitted by the presence of a day-to-night wind of 4.4 −2.2 +1.8 km s −1 , while the retrieved equatorial jet velocity of 1.0 −1.8 +0.9 km s −1 is consistent with the absence of such a jet. Such a wind pattern is consistent with the observed line broadening and can explain the majority of the velocity offset, while uncertainties in the ephemerides and the effects of a hot spot could also contribute to this offset. We further retrieved an inverted temperature-pressure profile, and under the assumption of equilibrium chemistry we retrieved a C/O ratio of 0.32 −0.14 +0.41 and a metallicity of M/H = 1.40 −0.60 +1.39 . Conclusions . We showed that red-shifts of a few km s −1 in the dayside spectra could be explained by day-to-night winds. Further studies combining transmission and dayside observations could advance our understanding of WASP-189 b’s atmospheric circulation by improving the uncertainties in the velocity offset and wind parameters.

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Publication Details

Journal
Astronomy and Astrophysics
Published
2024-11-29
DOI
https://doi.org/10.1051/0004-6361/202451391
Citations
15
Primary Topic
Geophysics and Gravity Measurements
Type
article
Field-Weighted Citation Impact
7.21
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article

Retrieving wind properties from the ultra-hot dayside of WASP-189 b with CRIRES+

A. Reiners, F. Lesjak, E. Nagel, U. Seemann et al.
15 citations
Astronomy and Astrophysics
Geophysics and Gravity Measurements
7.21
article

Retrieving wind properties from the ultra-hot dayside of WASP-189 b with CRIRES+

A. Reiners, F. Lesjak, E. Nagel, U. Seemann, D. Cont, D. Shulyak, Adam D. Rains, A. P. Hatzes, A. Lavail, L. Nortmann, L. Boldt-Christmas, F. Yan, S. Czesla, Nikolai E. Piskunov, M. Rengel
article en
15 citations

Abstract

Context . The extreme temperature gradients from day- to nightside in the atmospheres of hot Jupiters generate fast winds in the form of equatorial jets or day-to-night flows. Observations of blue-shifted and red-shifted signals in the transmission and dayside spectra of WASP-189 b have sparked discussions about the nature of winds on this planet. Aims . To investigate the structure of winds in the atmosphere of the ultra-hot Jupiter WASP-189 b, we studied its dayside emission spectrum with CRIRES + in the spectral K band. Methods . After removing stellar and telluric lines, we used the cross-correlation method to search for a range of molecules and detected emission signals of CO and Fe. Subsequently, we employed a Bayesian framework to retrieve the atmospheric parameters relating to the temperature–pressure structure and chemistry, and incorporated a numerical model of the line profile influenced by various dynamic effects to determine the wind structure. Results . The cross-correlation signals of CO and Fe showed a velocity offset of ~6 km s −1 , which could be caused by a fast day-tonight wind in the atmosphere of WASP-189 b. The atmospheric retrieval showed that the line profile of the observed spectra is best fitted by the presence of a day-to-night wind of 4.4 −2.2 +1.8 km s −1 , while the retrieved equatorial jet velocity of 1.0 −1.8 +0.9 km s −1 is consistent with the absence of such a jet. Such a wind pattern is consistent with the observed line broadening and can explain the majority of the velocity offset, while uncertainties in the ephemerides and the effects of a hot spot could also contribute to this offset. We further retrieved an inverted temperature-pressure profile, and under the assumption of equilibrium chemistry we retrieved a C/O ratio of 0.32 −0.14 +0.41 and a metallicity of M/H = 1.40 −0.60 +1.39 . Conclusions . We showed that red-shifts of a few km s −1 in the dayside spectra could be explained by day-to-night winds. Further studies combining transmission and dayside observations could advance our understanding of WASP-189 b’s atmospheric circulation by improving the uncertainties in the velocity offset and wind parameters.

Astronomy and AstrophysicsVol. 693
Uppsala University (SE), University of Science and Technology of China (CN), Centre National de la Recherche Scientifique (FR), European Southern Observatory (DE), Université Fédérale de Toulouse Midi-Pyrénées (FR), Excellence Cluster Origins (DE), Max Planck Institute for Solar System Research (DE), Thüringer Landessternwarte Tautenburg (DE), Instituto de Astrofísica de Andalucía (ES), Institut de Recherche en Astrophysique et Planétologie (FR), University of Göttingen (DE), Ludwig-Maximilians-Universität München (DE)
Openalex Percentile: Top 2%
Geophysics and Gravity Measurements
7.21
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