{"@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/1360574096148458752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/ja095ia02p01061"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJA095iA02p01061"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JA095iA02p01061"}}],"dc:title":[{"@value":"Global measures of ionospheric electrodynamic activity inferred from combined incoherent scatter radar and ground magnetometer observations"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>An analysis of several global measures of high‐latitude ionospheric electrodynamic activity is undertaken on the basis of results obtained from the Assimilative Mapping of Ionospheric Electrodynamics (AMIE) procedure applied to incoherent scatter radar and ground magnetometer observations for January 18–19, 1984. Different global measures of electric potentials, currents, resistances, and energy transfer from the magnetosphere show temporal variations that are generally well correlated. We present parameterizations of these quantities in terms of the <jats:italic>AE</jats:italic> index and the hemispheric power index of precipitating auroral particles. It is shown how error estimates of the mapped electric fields can be used to correct the estimation of Joule heating. Global measures of potential drop, field‐aligned current, and Joule heating as obtained by the AMIE procedure are compared with similar measures presented in previous studies. Agreement is found to within the uncertainties inherent in each study. The mean potential drop through which field‐aligned currents flow in closing through the ionosphere is approximately 28% of the total polar cap potential drop under all conditions during these 2 days. We note that order‐of‐magnitude differences can appear when comparing different global measures of total electric current flow and of effective resistances of the global circuit, so that care must be exercised in choosing characteristic values of these parameters for circuit‐analogy studies of ionosphere‐magnetosphere electrodynamic coupling.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380567186807887875","@type":"Researcher","foaf:name":[{"@value":"A. D. Richmond"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458755","@type":"Researcher","foaf:name":[{"@value":"Y. Kamide"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861293934304000","@type":"Researcher","foaf:name":[{"@value":"S.‐I. Akasofu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458753","@type":"Researcher","foaf:name":[{"@value":"D. Alcaydé"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458756","@type":"Researcher","foaf:name":[{"@value":"M. Blanc"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458628","@type":"Researcher","foaf:name":[{"@value":"O. de la Beaujardière"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458624","@type":"Researcher","foaf:name":[{"@value":"D. S. Evans"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458629","@type":"Researcher","foaf:name":[{"@value":"J. C. Foster"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861293934304001","@type":"Researcher","foaf:name":[{"@value":"E. Friis‐Christensen"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458757","@type":"Researcher","foaf:name":[{"@value":"J. M. Holt"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458625","@type":"Researcher","foaf:name":[{"@value":"R. J. Pellinen"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458626","@type":"Researcher","foaf:name":[{"@value":"C. Senior"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574096148458754","@type":"Researcher","foaf:name":[{"@value":"A. N. Zaitzev"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Space Physics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1990-02","prism:volume":"95","prism:number":"A2","prism:startingPage":"1061","prism:endingPage":"1071"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJA095iA02p01061"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JA095iA02p01061"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282813187215104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"New diagnosis for energy flow from solar wind to ionosphere during substorm: Global MHD simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564288163925760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simulation study of near-Earth space disturbances: 2. Auroral substorms"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564288163926784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Energy flow exciting field-aligned current at substorm expansion onset"},{"@value":"Energy Flow Exciting Field‐Aligned Current at Substorm Expansion Onset"}]},{"@id":"https://cir.nii.ac.jp/crid/1050572512051726464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evolution of auroral substorm as viewed from MHD simulations: dynamics, energy transfer and energy conversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1050859073008347136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Generation of Field-Aligned Currents During Substorm Expansion: An Update"},{"@value":"Generation of Field‐Aligned Currents During Substorm Expansion: An Update"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/ja095ia02p01061"},{"@type":"CROSSREF","@value":"10.1029/2018ja026177_references_DOI_97xqzRjFfQ76c6YHcElpJEtslRK"},{"@type":"CROSSREF","@value":"10.1029/2022ja031011_references_DOI_97xqzRjFfQ76c6YHcElpJEtslRK"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0273-2_references_DOI_97xqzRjFfQ76c6YHcElpJEtslRK"},{"@type":"CROSSREF","@value":"10.1002/2017ja024294_references_DOI_97xqzRjFfQ76c6YHcElpJEtslRK"},{"@type":"CROSSREF","@value":"10.1007/s41614-019-0037-x_references_DOI_97xqzRjFfQ76c6YHcElpJEtslRK"}]}