{"@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/1362825895048372224.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/98ja02656"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98JA02656"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98JA02656"}}],"dc:title":[{"@value":"Modeling investigation of the evening prereversal enhancement of the zonal electric field in the equatorial ionosphere"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The neutral winds in the <jats:italic>E</jats:italic> and <jats:italic>F</jats:italic> regions are the drivers of the low‐latitude ionospheric current system and observed electric field structure. A flux‐tube‐integrated model of ionospheric electrodynamics is used to examine three proposed causes of the prereversal enhancement of the zonal electric field. All three mechanisms try to define the obscure relationship between the <jats:italic>F</jats:italic> region dynamo and the evening prereversal enhancement. The results show that the original mechanism proposed by <jats:italic>Rishbeth</jats:italic> [1971] is the fundamental mechanism. The rapid change in the vertical polarization electric field near local sunset, which is due to the accelerating neutral wind dynamo, produces a corresponding change in the zonal electric field through curl‐free requirements. The other two mechanisms do not produce the evening enhancement but alter the enhancement shape and magnitude.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895048372224","@type":"Researcher","foaf:name":[{"@value":"J. Vincent Eccles"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Space Physics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1998-11","prism:volume":"103","prism:number":"A11","prism:startingPage":"26709","prism:endingPage":"26719"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98JA02656"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98JA02656"}],"createdAt":"2004-02-03","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002216707178112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrodynamics of the formation of ionospheric wave number 4 longitudinal structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229802359296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Explicit characteristics of evolutionary‐type plasma bubbles observed from Equatorial Atmosphere Radar during the low to moderate solar activity years 2010–2012"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021389806439808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Assessing the potential of ionosonde for forecasting post-sunset equatorial spread F: an observational experiment in Southeast Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390556483840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Equinoctial asymmetry of plasma bubble occurrence and electric field at evening: GPS and ionosonde measurements in Southeast Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942135631488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Unseasonal development of post-sunset F-region irregularities over Southeast Asia on 28 July 2014 : 2. Forcing from below？"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892082797824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Post-sunset rise of equatorial F layer-or upwelling growth？"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/98ja02656"},{"@type":"CROSSREF","@value":"10.1029/2008ja013301_references_DOI_JyMhc62JiAZPXXqx2FdB3ZxxbH3"},{"@type":"CROSSREF","@value":"10.1002/2014ja020878_references_DOI_JyMhc62JiAZPXXqx2FdB3ZxxbH3"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0218-1_references_DOI_JyMhc62JiAZPXXqx2FdB3ZxxbH3"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01941-1_references_DOI_JyMhc62JiAZPXXqx2FdB3ZxxbH3"},{"@type":"CROSSREF","@value":"10.1016/j.jastp.2023.106136_references_DOI_JyMhc62JiAZPXXqx2FdB3ZxxbH3"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0179-4_references_DOI_JyMhc62JiAZPXXqx2FdB3ZxxbH3"}]}