{"@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/1363388844756273280.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005ja011021"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005JA011021"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005JA011021"}}],"dc:title":[{"@value":"Stormtime coupling of the ring current, plasmasphere, and topside ionosphere: Electromagnetic and plasma disturbances"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We compare plasma and field disturbances observed in the ring current/plasmasphere overlap region and in the conjugate ionosphere during the magnetic storm of 5 June 1991. Data come from the Combined Release and Radiation Effects Satellite (CRRES) flying in a geostationary transfer orbit and three satellites of the Defense Meteorological Satellite Program (DMSP) series in Sun‐synchronous polar orbits. In the region between ring current nose structures and the electron plasma sheet, CRRES detected wave‐like features in local electric and magnetic fields, embedded in structured cold plasmas. Mapped to the ionosphere, these fields should reflect structuring within subauroral plasma streams (SAPS). Indeed, during the period of interest, DMSP F8, F9, and F10 satellites observed highly structured SAPS in the evening ionosphere at topside altitudes. They were collocated with precipitating ring current ions, enhanced fluxes of suprathermal electrons and ions, elevated electron temperatures, and irregular plasma density troughs. Overall, these events are similar to electromagnetic structures observed by DMSP satellites within SAPS during recent geomagnetic storms (Mishin et al., 2003, 2004). Their features can be explained in terms of Alfvén and fast magnetosonic perturbations. We developed a scenario for the formation of elevated electron temperatures at the equatorward side of the SAPS. It includes a lower‐hybrid drift instability driven by diamagnetic currents, consistent with strong lower‐ and upper‐hybrid plasma wave activity and intense fluxes of the low‐energy electrons and ions near the ring current's inner edge.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844756273280","@type":"Researcher","foaf:name":[{"@value":"E. V. Mishin"}],"jpcoar:affiliationName":[{"@value":"Institute for Scientific Research Boston College  Chestnut Hill Massachusetts USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579816980270720","@type":"Researcher","foaf:name":[{"@value":"W. J. Burke"}],"jpcoar:affiliationName":[{"@value":"Space Vehicles Directorate Air Force Research Laboratory  Hanscom Air Force Base Massachusetts USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Space Physics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2005-07","prism:volume":"110","prism:number":"A7"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005JA011021"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005JA011021"}],"createdAt":"2005-07-10","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050571547597131264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Multi‐Wavelength Imaging Observations of STEVE at Athabasca, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294740630218368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multi‐Scale Density Structures in the Plasmaspheric Plume During a Geomagnetic Storm"}]},{"@id":"https://cir.nii.ac.jp/crid/1390869987442216960","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Natural Phenomena Occurring in the Earth’s Environment via a Prism of MaLAIM Coupling Mechanism"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842044692096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Review of the accomplishments of midlatitude Super Dual Auroral Radar Network (SuperDARN) HF radars"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005ja011021"},{"@type":"CROSSREF","@value":"10.1029/2020ja028622_references_DOI_KBmcGpXOBtYmKgmgwTi3TySSxJs"},{"@type":"CROSSREF","@value":"10.1029/2021ja030230_references_DOI_KBmcGpXOBtYmKgmgwTi3TySSxJs"},{"@type":"CROSSREF","@value":"10.1541/jae.45.1_references_DOI_KBmcGpXOBtYmKgmgwTi3TySSxJs"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0270-5_references_DOI_KBmcGpXOBtYmKgmgwTi3TySSxJs"}]}