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Intradecadal variations in length of day and their correspondence with geomagnetic jerks
Earth’s core oscillations and magnetic field inside the liquid outer core cannot be observed directly from the surface, we can infer these information from the intradecadal variations in Earth’s rotation rate defined by length of day. However, the fine time-varying characteristics as well as relevan...
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Published in: | Nature communications 2020-05, Vol.11 (1), p.2273-2273, Article 2273 |
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description | Earth’s core oscillations and magnetic field inside the liquid outer core cannot be observed directly from the surface, we can infer these information from the intradecadal variations in Earth’s rotation rate defined by length of day. However, the fine time-varying characteristics as well as relevant mechanisms of the intradecadal variations are still unclear. Here we report that the intradecadal variations present a significant 8.6-year harmonic component with an unexpected increasing phenomenon, besides a 6-year decreasing oscillation. More importantly, we find that there is a very good correspondence between the extremes of the 8.6-year oscillation with geomagnetic jerks. The fast equatorial waves with subdecadal periods propagating at Earth’s core surface may explain the origin of this 8.6-year oscillation.
Earth rotation variation reflects the physics, dynamics and the magnetic field changes of Earth’s interior. The authors find a significant ~8.6 year periodic increasing oscillation in length of day and its good link to geomagnetic jerks related to Earth’s core oscillations, which may be used to predict the future jerk timings. |
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Earth rotation variation reflects the physics, dynamics and the magnetic field changes of Earth’s interior. The authors find a significant ~8.6 year periodic increasing oscillation in length of day and its good link to geomagnetic jerks related to Earth’s core oscillations, which may be used to predict the future jerk timings.</description><identifier>ISSN: 2041-1723</identifier><identifier>EISSN: 2041-1723</identifier><identifier>DOI: 10.1038/s41467-020-16109-8</identifier><identifier>PMID: 32385238</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>639/33/445/210 ; 704/2151/2809 ; Earth core ; Earth rotation ; Earth surface ; Geomagnetic field ; Geomagnetism ; Humanities and Social Sciences ; Magnetic fields ; multidisciplinary ; Oscillations ; Science ; Science (multidisciplinary) ; Variation ; Wave propagation</subject><ispartof>Nature communications, 2020-05, Vol.11 (1), p.2273-2273, Article 2273</ispartof><rights>The Author(s) 2020</rights><rights>The Author(s) 2020. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c540t-c44fb26d71e7b6ce94625d9b6f62f238a7780b1eacd93ab1334d5c892df48fff3</citedby><cites>FETCH-LOGICAL-c540t-c44fb26d71e7b6ce94625d9b6f62f238a7780b1eacd93ab1334d5c892df48fff3</cites><orcidid>0000-0002-3474-0360 ; 0000-0002-1365-0577</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2400096859/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2400096859?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,885,25753,27924,27925,37012,37013,44590,53791,53793,75126</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/32385238$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Duan, Pengshuo</creatorcontrib><creatorcontrib>Huang, Chengli</creatorcontrib><title>Intradecadal variations in length of day and their correspondence with geomagnetic jerks</title><title>Nature communications</title><addtitle>Nat Commun</addtitle><addtitle>Nat Commun</addtitle><description>Earth’s core oscillations and magnetic field inside the liquid outer core cannot be observed directly from the surface, we can infer these information from the intradecadal variations in Earth’s rotation rate defined by length of day. However, the fine time-varying characteristics as well as relevant mechanisms of the intradecadal variations are still unclear. Here we report that the intradecadal variations present a significant 8.6-year harmonic component with an unexpected increasing phenomenon, besides a 6-year decreasing oscillation. More importantly, we find that there is a very good correspondence between the extremes of the 8.6-year oscillation with geomagnetic jerks. The fast equatorial waves with subdecadal periods propagating at Earth’s core surface may explain the origin of this 8.6-year oscillation.
Earth rotation variation reflects the physics, dynamics and the magnetic field changes of Earth’s interior. 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Earth rotation variation reflects the physics, dynamics and the magnetic field changes of Earth’s interior. The authors find a significant ~8.6 year periodic increasing oscillation in length of day and its good link to geomagnetic jerks related to Earth’s core oscillations, which may be used to predict the future jerk timings.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>32385238</pmid><doi>10.1038/s41467-020-16109-8</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-3474-0360</orcidid><orcidid>https://orcid.org/0000-0002-1365-0577</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | 639/33/445/210 704/2151/2809 Earth core Earth rotation Earth surface Geomagnetic field Geomagnetism Humanities and Social Sciences Magnetic fields multidisciplinary Oscillations Science Science (multidisciplinary) Variation Wave propagation |
title | Intradecadal variations in length of day and their correspondence with geomagnetic jerks |
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