Is the atmosphere of the ultra-hot Jupiter WASP-121b variable?

Fuente: arXiv
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Autori principali: Changeat, Quentin, Skinner, Jack W., Cho, James Y-K., Nättilä, Joonas, Waldmann, Ingo P., Al-Refaie, Ahmed F., Dyrek, Achrène, Edwards, Billy, Mikal-Evans, Thomas, Joshua, Max, Morello, Giuseppe, Skaf, Nour, Tsiaras, Angelos, Venot, Olivia, Yip, Kai Hou
Natura: Preprint
Pubblicazione: 2024
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author Changeat, Quentin
Skinner, Jack W.
Cho, James Y-K.
Nättilä, Joonas
Waldmann, Ingo P.
Al-Refaie, Ahmed F.
Dyrek, Achrène
Edwards, Billy
Mikal-Evans, Thomas
Joshua, Max
Morello, Giuseppe
Skaf, Nour
Tsiaras, Angelos
Venot, Olivia
Yip, Kai Hou
author_facet Changeat, Quentin
Skinner, Jack W.
Cho, James Y-K.
Nättilä, Joonas
Waldmann, Ingo P.
Al-Refaie, Ahmed F.
Dyrek, Achrène
Edwards, Billy
Mikal-Evans, Thomas
Joshua, Max
Morello, Giuseppe
Skaf, Nour
Tsiaras, Angelos
Venot, Olivia
Yip, Kai Hou
contents We present a comprehensive analysis of the Hubble Space Telescope observations of the atmosphere of WASP-121 b, a ultra-hot Jupiter. After reducing the transit, eclipse, and phase-curve observations with a uniform methodology and addressing the biases from instrument systematics, sophisticated atmospheric retrievals are used to extract robust constraints on the thermal structure, chemistry, and cloud properties of the atmosphere. Our analysis shows that the observations are consistent with a strong thermal inversion beginning at ~0.1 bar on the dayside, solar to subsolar metallicity Z (i.e., -0.77 < log(Z) < 0.05), and super-solar C/O ratio (i.e., 0.59 < C/O < 0.87). More importantly, utilizing the high signal-to-noise ratio and repeated observations of the planet, we identify the following unambiguous time-varying signals in the data: i) a shift of the putative hotspot offset between the two phase-curves and ii) varying spectral signatures in the transits and eclipses. By simulating the global dynamics of WASP-121 b atmosphere at high-resolution, we show that the identified signals are consistent with quasi-periodic weather patterns, hence atmospheric variability, with signatures at the level probed by the observations (~5% to ~10%) that change on a timescale of ~5 planet days; in the simulations, the weather patterns arise from the formation and movement of storms and fronts, causing hot (as well as cold) patches of atmosphere to deform, separate, and mix in time.
format Preprint
id arxiv_https___arxiv_org_abs_2401_01465
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Is the atmosphere of the ultra-hot Jupiter WASP-121b variable?
Changeat, Quentin
Skinner, Jack W.
Cho, James Y-K.
Nättilä, Joonas
Waldmann, Ingo P.
Al-Refaie, Ahmed F.
Dyrek, Achrène
Edwards, Billy
Mikal-Evans, Thomas
Joshua, Max
Morello, Giuseppe
Skaf, Nour
Tsiaras, Angelos
Venot, Olivia
Yip, Kai Hou
Earth and Planetary Astrophysics
We present a comprehensive analysis of the Hubble Space Telescope observations of the atmosphere of WASP-121 b, a ultra-hot Jupiter. After reducing the transit, eclipse, and phase-curve observations with a uniform methodology and addressing the biases from instrument systematics, sophisticated atmospheric retrievals are used to extract robust constraints on the thermal structure, chemistry, and cloud properties of the atmosphere. Our analysis shows that the observations are consistent with a strong thermal inversion beginning at ~0.1 bar on the dayside, solar to subsolar metallicity Z (i.e., -0.77 < log(Z) < 0.05), and super-solar C/O ratio (i.e., 0.59 < C/O < 0.87). More importantly, utilizing the high signal-to-noise ratio and repeated observations of the planet, we identify the following unambiguous time-varying signals in the data: i) a shift of the putative hotspot offset between the two phase-curves and ii) varying spectral signatures in the transits and eclipses. By simulating the global dynamics of WASP-121 b atmosphere at high-resolution, we show that the identified signals are consistent with quasi-periodic weather patterns, hence atmospheric variability, with signatures at the level probed by the observations (~5% to ~10%) that change on a timescale of ~5 planet days; in the simulations, the weather patterns arise from the formation and movement of storms and fronts, causing hot (as well as cold) patches of atmosphere to deform, separate, and mix in time.
title Is the atmosphere of the ultra-hot Jupiter WASP-121b variable?
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2401.01465