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Jupiter's atmospheric jet streams extend thousands of kilometres deep

机译:木星的大气射流深达数千公里

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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.
机译:木星观测到的东西向射流延伸的深度是一个长期存在的问题(1,2)。自从2016年7月以来一直围绕着这颗天然气巨星运行的朱诺航天器(3,4),解决这个难题一直是其主要目标。朱诺的引力测量结果显示木星的引力场是南北不对称的(5),是行星大气和内部流动的标志(6)。在这里我们报告说,测得的奇重力谐波J(3),J(5),J(7)和J(9)表明,观察到的喷射流(出现在云层)向下延伸到数千距离云层以下约9公里,可能到约3000公里深度的磁耗散区域(7,8)。通过将测得的重力值转化为风场(9),我们可以计算出最可能的深层大气和内部流的垂直剖面及其深度的纬度依赖性。此外,当考虑到内部结构(10)的影响时,由这种流动曲线产生的偶数重力谐波J(8)和J(10)也与测量值匹配。这些结果表明,动态大气的质量约为木星总质量的百分之一。

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  • 来源
    《Nature》 |2018年第7695期|223-226|共4页
  • 作者单位

    Weizmann Inst Sci, Dept Earth & Planetary Sci, IL-76100 Rehovot, Israel;

    Weizmann Inst Sci, Dept Earth & Planetary Sci, IL-76100 Rehovot, Israel;

    Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA;

    Southwest Res Inst, San Antonio, TX 78238 USA;

    Sapienza Univ Roma, Dept Mech & Aerosp Engn, I-00184 Rome, Italy;

    Univ Cote dAzur, Lagrange CNRS, OCA, F-06304 Nice, France;

    Harvard Univ, Dept Earth & Planetary Sci, 20 Oxford St, Cambridge, MA 02138 USA;

    Space Res Corp, Annapolis, MD 21403 USA;

    CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA;

    Sapienza Univ Roma, Dept Mech & Aerosp Engn, I-00184 Rome, Italy;

    CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA;

    Univ Zurich, Ctr Theoret Astrophys & Cosmol, Inst Computat Sci, CH-8057 Zurich, Switzerland;

    CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA;

    CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA;

    Cornell Univ, Dept Astron, Ithaca, NY 14853 USA;

    Univ Cote dAzur, Lagrange CNRS, OCA, F-06304 Nice, France;

    Univ Calif Berkeley, Dept Earth & Planetray Sci, Berkeley, CA 94720 USA;

    Univ Calif Berkeley, Dept Earth & Planetray Sci, Berkeley, CA 94720 USA;

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  • 入库时间 2022-08-18 02:51:28

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