Jupiter's inhomogeneous envelope
Autor: | Y. Miguel, M. Bazot, T. Guillot, S. Howard, E. Galanti, Y. Kaspi, W. B. Hubbard, B. Militzer, R. Helled, S. K. Atreya, J. E. P. Connerney, D. Durante, L. Kulowski, J. I. Lunine, D. Stevenson, S. Bolton |
---|---|
Jazyk: | angličtina |
Rok vydání: | 2022 |
Předmět: |
Earth and Planetary Astrophysics (astro-ph.EP)
composition Astrophysics - Earth and Planetary Astrophysics Astrophysics - Solar and Stellar Astrophysics Juppiter planets and satellites: interiors gaseous planets formation composition formation planets and satellites planets and satellites FOS: Physical sciences Astronomy and Astrophysics gaseous planets planets and satellites interiors planets and satellites interiors Astrophysics - Solar and Stellar Astrophysics Space and Planetary Science Physics::Space Physics Astrophysics::Earth and Planetary Astrophysics Solar and Stellar Astrophysics (astro-ph.SR) Astrophysics - Earth and Planetary Astrophysics |
Zdroj: | Astronomy & Astrophysics, 662:A18 |
Popis: | While Jupiter's massive gas envelope consists mainly of hydrogen and helium, the key to understanding Jupiter's formation and evolution lies in the distribution of the remaining (heavy) elements. Before the Juno mission, the lack of high-precision gravity harmonics precluded the use of statistical analyses in a robust determination of the heavy-elements distribution in Jupiter's envelope. In this paper, we assemble the most comprehensive and diverse collection of Jupiter interior models to date and use it to study the distribution of heavy elements in the planet's envelope. We apply a Bayesian statistical approach to our interior model calculations, reproducing the Juno gravitational and atmospheric measurements and constraints from the deep zonal flows. Our results show that the gravity constraints lead to a deep entropy of Jupiter corresponding to a 1 bar temperature 5-15 K higher than traditionally assumed. We also find that uncertainties in the equation of state are crucial when determining the amount of heavy elements in Jupiter's interior. Our models put an upper limit to the inner compact core of Jupiter of 7 Earth masses, independently on the structure model (with or without dilute core) and the equation of state considered. Furthermore, we robustly demonstrate that Jupiter's envelope is inhomogenous, with a heavy-element enrichment in the interior relative to the outer envelope. This implies that heavy element enrichment continued through the gas accretion phase, with important implications for the formation of giant planets in our solar system and beyond. Accepted for publication in A&A |
Databáze: | OpenAIRE |
Externí odkaz: |