{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361699995576348032.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011eo020002"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011EO020002"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2011EO020002"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2011EO020002"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011EO020002"}}],"dc:title":[{"@value":"Observation of Magnetic Fields Generated by Tsunamis"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Tsunamis produce perturbations in the Earth's magnetic field by electromagnetic induction. Recent deployments of highly accurate magnetometers and the exceptionally deep solar minimum provided ideal conditions to observe these small signals from the tsunami resulting from the strong Chilean earthquake on 27 February 2010. Magnetic observatory measurements on Easter Island, 3500 kilometers west of the epicenter, show a periodic signal of 1 nanotesla, coincident in time with recordings from the local tide gauge. The detection of these magnetic signals represents a milestone in understanding tsunami‐induced electromagnetic effects.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995576348033","@type":"Researcher","foaf:name":[{"@value":"Chandrasekharan Manoj"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995576348034","@type":"Researcher","foaf:name":[{"@value":"Stefan Maus"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995576348032","@type":"Researcher","foaf:name":[{"@value":"Arnaud Chulliat"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00963941"},{"@type":"EISSN","@value":"23249250"}],"prism:publicationName":[{"@value":"Eos, Transactions American Geophysical Union"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2011-01-11","prism:volume":"92","prism:number":"2","prism:startingPage":"13","prism:endingPage":"14"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011EO020002"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2011EO020002"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2011EO020002"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011EO020002"}],"createdAt":"2011-01-24","modifiedAt":"2023-09-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050583402767207168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"TIARES Project -Tomographic investigation by seafloor array experiment for the Society hotspot"},{"@value":"TIARES Project—Tomographic investigation by seafloor array experiment for the 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