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dc.contributor.authorKong, D
dc.contributor.authorZhang, K
dc.contributor.authorSchubert, G
dc.date.accessioned2016-06-06T08:44:44Z
dc.date.issued2016-03-23
dc.description.abstractConvective motion in the deep metallic hydrogen region of Jupiter is believed to generate its magnetic field, the strongest in the solar system. The amplitude, structure and depth of the convective motion are unknown. A promising way of probing the Jovian convective dynamo is to measure its effect on the external gravitational field, a task to be soon undertaken by the Juno spacecraft. We calculate the gravitational signature of non-axisymmetric convective motion in the Jovian metallic hydrogen region and show that with sufficiently accurate measurements it can reveal the nature of the deep convection.en_GB
dc.description.sponsorshipKZ is supported by Leverhulme Trust Research Project Grant RPG-2015-096 and by Macau FDCT grant 039/2013/A2. The computation made use of the high performance computing resources in the Core Facility for Advanced Research Computing at Shanghai Astronomical Observatory, Chinese Academy of Sciences.en_GB
dc.identifier.citationVol. 6, article 23497en_GB
dc.identifier.doi10.1038/srep23497
dc.identifier.urihttp://hdl.handle.net/10871/21845
dc.language.isoenen_GB
dc.publisherNature Publishing Groupen_GB
dc.relation.urlhttp://www.ncbi.nlm.nih.gov/pubmed/27005472en_GB
dc.rightsOpen access. This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/en_GB
dc.titleUsing Jupiter's gravitational field to probe the Jovian convective dynamoen_GB
dc.typeArticleen_GB
dc.date.available2016-06-06T08:44:44Z
exeter.place-of-publicationEngland
dc.descriptionThis is the final version of the article. Available from Nature Publishing Group via the DOI in this record.en_GB
dc.identifier.journalScientific Reportsen_GB


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