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A suppression of differential rotation in Jupiter's deep interior.
Guillot, T; Miguel, Y; Militzer, B; Hubbard, W B; Kaspi, Y; Galanti, E; Cao, H; Helled, R; Wahl, S M; Iess, L; Folkner, W M; Stevenson, D J; Lunine, J I; Reese, D R; Biekman, A; Parisi, M; Durante, D; Connerney, J E P; Levin, S M; Bolton, S J.
Afiliação
  • Guillot T; Université Côte d'Azur, OCA, Lagrange CNRS, 06304 Nice, France.
  • Miguel Y; Université Côte d'Azur, OCA, Lagrange CNRS, 06304 Nice, France.
  • Militzer B; Leiden Observatory, University of Leiden, Niels Bohrweg 2, 2333CA Leiden, The Netherlands.
  • Hubbard WB; University of California, Berkeley, California 94720, USA.
  • Kaspi Y; Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona 85721, USA.
  • Galanti E; Weizmann Institute of Science, Rehovot 76100, Israel.
  • Cao H; Weizmann Institute of Science, Rehovot 76100, Israel.
  • Helled R; California Institute of Technology, Pasadena, California 91125, USA.
  • Wahl SM; Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA.
  • Iess L; University of Zurich, 8057 Zurich, Switzerland.
  • Folkner WM; University of California, Berkeley, California 94720, USA.
  • Stevenson DJ; Sapienza Università di Roma, 00184 Rome, Italy.
  • Lunine JI; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, USA.
  • Reese DR; California Institute of Technology, Pasadena, California 91125, USA.
  • Biekman A; Cornell University, Ithaca, New York 14853, USA.
  • Parisi M; LESIA, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universités, UPMC Université Paris 06, Université Paris Diderot, Sorbonne Paris Cité, 92195 Meudon, France.
  • Durante D; Université Côte d'Azur, OCA, Lagrange CNRS, 06304 Nice, France.
  • Connerney JEP; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, USA.
  • Levin SM; Sapienza Università di Roma, 00184 Rome, Italy.
  • Bolton SJ; NASA/GSFC, Greenbelt, Maryland, USA.
Nature ; 555(7695): 227-230, 2018 03 07.
Article em En | MEDLINE | ID: mdl-29517000
ABSTRACT
Jupiter's atmosphere is rotating differentially, with zones and belts rotating at speeds that differ by up to 100 metres per second. Whether this is also true of the gas giant's interior has been unknown, limiting our ability to probe the structure and composition of the planet. The discovery by the Juno spacecraft that Jupiter's gravity field is north-south asymmetric and the determination of its non-zero odd gravitational harmonics J3, J5, J7 and J9 demonstrates that the observed zonal cloud flow must persist to a depth of about 3,000 kilometres from the cloud tops. Here we report an analysis of Jupiter's even gravitational harmonics J4, J6, J8 and J10 as observed by Juno and compared to the predictions of interior models. We find that the deep interior of the planet rotates nearly as a rigid body, with differential rotation decreasing by at least an order of magnitude compared to the atmosphere. Moreover, we find that the atmospheric zonal flow extends to more than 2,000 kilometres and to less than 3,500 kilometres, making it fully consistent with the constraints obtained independently from the odd gravitational harmonics. This depth corresponds to the point at which the electric conductivity becomes large and magnetic drag should suppress differential rotation. Given that electric conductivity is dependent on planetary mass, we expect the outer, differentially rotating region to be at least three times deeper in Saturn and to be shallower in massive giant planets and brown dwarfs.

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Tipo de estudo: Prognostic_studies Idioma: En Revista: Nature Ano de publicação: 2018 Tipo de documento: Article País de afiliação: França

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Tipo de estudo: Prognostic_studies Idioma: En Revista: Nature Ano de publicação: 2018 Tipo de documento: Article País de afiliação: França