Jupiter's atmospheric jet streams extend thousands of kilometres deep

被引:199
作者
Kaspi, Y. [1 ]
Galanti, E. [1 ]
Hubbard, W. B. [2 ,3 ]
Stevenson, D. J.
Bolton, S. J. [4 ]
Iess, L. [5 ]
Guillot, T. [6 ]
Bloxham, J. [7 ]
Connerney, J. E. P. [8 ,9 ]
Cao, H. [3 ,7 ]
Durante, D. [5 ]
Folkner, W. M. [10 ]
Helled, R. [11 ]
Ingersoll, A. P. [3 ]
Levin, S. M. [10 ]
Lunine, J. I. [12 ]
Miguel, Y. [6 ,13 ]
Militzer, B. [14 ]
Parisi, M.
Wahl, S. M. [14 ]
机构
[1] Weizmann Inst Sci, Dept Earth & Planetary Sci, IL-76100 Rehovot, Israel
[2] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA
[3] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[4] Southwest Res Inst, San Antonio, TX 78238 USA
[5] Sapienza Univ Roma, Dept Mech & Aerosp Engn, I-00184 Rome, Italy
[6] Univ Cote dAzur, Lagrange CNRS, OCA, F-06304 Nice, France
[7] Harvard Univ, Dept Earth & Planetary Sci, 20 Oxford St, Cambridge, MA 02138 USA
[8] Space Res Corp, Annapolis, MD 21403 USA
[9] NASA, GSFC, Greenbelt, MD 20771 USA
[10] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA
[11] Univ Zurich, Ctr Theoret Astrophys & Cosmol, Inst Computat Sci, CH-8057 Zurich, Switzerland
[12] Cornell Univ, Dept Astron, Ithaca, NY 14853 USA
[13] Leiden Univ, Leiden Observ, Leiden, Netherlands
[14] Univ Calif Berkeley, Dept Earth & Planetray Sci, Berkeley, CA 94720 USA
基金
美国国家科学基金会;
关键词
ODD GRAVITATIONAL HARMONICS; ZONAL-WIND-PROFILE; GIANT PLANETS; GRAVITY; DYNAMICS; GALILEO; FLOWS;
D O I
10.1038/nature25793
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The depth to which Jupiter's observed east-west jet streams extend has been a long-standing question(1,2). Resolving this puzzle has been a primary goal for the Juno spacecraft(3,4), which has been in orbit around the gas giant since July 2016. Juno's gravitational measurements have revealed that Jupiter's gravitational field is north-south asymmetric(5), which is a signature of the planet's atmospheric and interior flows(6). Here we report that the measured odd gravitational harmonics J(3), J(5), J(7) and J(9) indicate that the observed jet streams, as they appear at the cloud level, extend down to depths of thousands of kilometres beneath the cloud level, probably to the region of magnetic dissipation at a depth of about 3,000 kilometres(7,8). By inverting the measured gravity values into a wind field(9), we calculate the most likely vertical profile of the deep atmospheric and interior flow, and the latitudinal dependence of its depth. Furthermore, the even gravity harmonics J(8) and J(10) resulting from this flow profile also match the measurements, when taking into account the contribution of the interior structure(10). These results indicate that the mass of the dynamical atmosphere is about one per cent of Jupiter's total mass.
引用
收藏
页码:223 / +
页数:14
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