{"@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/1361137044951006720.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/90gl02789"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F90GL02789"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/90GL02789"}}],"dc:title":[{"@value":"Location and propagation of the magnetotail current disruption during substorm expansion: Analysis and simulation of an ISEE multi‐onset event"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Magnetic field variations measured onboard the ISEE‐1 spacecraft in the tail northern lobe (∼22 R<jats:sub>E</jats:sub> geocentric distance) during a substorm with multiple onsets are analyzed and simulated using a model current sheet. This remote sensing study of the cross‐tail current sheet shows that substorm onsets are associated with a partial disruption of the cross‐tail current that begins in the near‐earth plasma sheet (∼7 R<jats:sub>E</jats:sub>) and that expands tailward during substorm expansion with a velocity of the order of 300 km/s. The two consecutive substorm onsets, which occur during a very active period (AE > 500 nT), correspond to a similar partial disruption of the near‐earth current sheet that expands tailwards over a distance of the order of 80 R<jats:sub>E</jats:sub>.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848482802884752","@type":"Researcher","foaf:name":[{"@value":"C. Jacquey"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044951006721","@type":"Researcher","foaf:name":[{"@value":"J. A. Sauvaud"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044951006848","@type":"Researcher","foaf:name":[{"@value":"J. Dandouras"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1991-03","prism:volume":"18","prism:number":"3","prism:startingPage":"389","prism:endingPage":"392"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F90GL02789"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/90GL02789"}],"createdAt":"2008-02-06","modifiedAt":"2023-11-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202065475968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnetic field dipolarization in the deep inner magnetosphere and its role in development of O"},{"@value":"Magnetic field dipolarization in the deep inner magnetosphere and its role in development of O<sup>+</sup>‐rich ring current"}]},{"@id":"https://cir.nii.ac.jp/crid/1050576282633237632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnetic Field and Energetic Particle Flux Oscillations and High-Frequency Waves Deep in the Inner Magnetosphere During Substorm Dipolarization: ERG Observations"},{"@value":"Magnetic Field and Energetic Particle Flux Oscillations and High‐Frequency Waves Deep in the Inner Magnetosphere During Substorm Dipolarization: ERG Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1050853038460209536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Severe Magnetic Fluctuations in the Near‐Earth Magnetotail: Spectral Analysis and Dependence on Solar Activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233288282368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetic reconnection X-line retreat associated with dipolarization of the Earth's magnetosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656365857280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electron Power-Law Spectra in Solar and Space Plasmas"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512467840","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Substorm-time magnetic field perturbations in the polar magnetosphere"},{"@value":"Substorm-time magnetic field perturbations in the polar magnetosphere: POLAR observations"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792003418368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of field-aligned current in the meridional plane during substorm : multipoint observations from satellites and ground stations"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/90gl02789"},{"@type":"CROSSREF","@value":"10.1029/2011gl049350_references_DOI_D4jWZzwTcPmewpSbztR31Ml10fp"},{"@type":"CROSSREF","@value":"10.1029/2010ja015321_references_DOI_D4jWZzwTcPmewpSbztR31Ml10fp"},{"@type":"CROSSREF","@value":"10.1029/2020ja029095_references_DOI_D4jWZzwTcPmewpSbztR31Ml10fp"},{"@type":"CROSSREF","@value":"10.1186/bf03352444_references_DOI_D4jWZzwTcPmewpSbztR31Ml10fp"},{"@type":"CROSSREF","@value":"10.1007/s11214-018-0515-4_references_DOI_D4jWZzwTcPmewpSbztR31Ml10fp"},{"@type":"CROSSREF","@value":"10.1029/2020ja027834_references_DOI_D4jWZzwTcPmewpSbztR31Ml10fp"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01182-6_references_DOI_D4jWZzwTcPmewpSbztR31Ml10fp"}]}