{"@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/1360004229804174208.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2015ja021799"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015JA021799"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA021799"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"West wall structuring of equatorial plasma bubbles simulated by three‐dimensional HIRB model"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Plasma density depletions in the equatorial ionosphere, or so‐called equatorial plasma bubbles (EPBs), are generated in the postsunset period and tend to have a very complex spatial structure. Especially, the east‐west asymmetry of EPBs has been reported by various observations. Using a high‐resolution bubble (HIRB) model, which is a newly developed three‐dimensional numerical model for the equatorial ionosphere, small‐scale structuring at the west wall of large‐scale <jats:italic>F</jats:italic> layer upwelling is clearly reproduced for the first time. It is not an eastward neutral wind but a vertical shear of zonal plasma drift velocity at the bottomside of the <jats:italic>F</jats:italic> region that plays an important role in accelerating the instability growth at the west wall and generating the east‐west asymmetry of EPBs.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229804174208","@type":"Researcher","foaf:name":[{"@value":"T. Yokoyama"}],"jpcoar:affiliationName":[{"@value":"National Institute of Information and Communications Technology  Koganei Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229804174338","@type":"Researcher","foaf:name":[{"@value":"H. Jin"}],"jpcoar:affiliationName":[{"@value":"National Institute of Information and Communications Technology  Koganei Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229804174209","@type":"Researcher","foaf:name":[{"@value":"H. Shinagawa"}],"jpcoar:affiliationName":[{"@value":"National Institute of Information and Communications Technology  Koganei Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699380"},{"@type":"EISSN","@value":"21699402"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Space Physics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2015-10","prism:volume":"120","prism:number":"10","prism:startingPage":"8810","prism:endingPage":"8816"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2015JA021799"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2015JA021799"}],"createdAt":"2015-11-23","modifiedAt":"2023-09-02","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256806024064","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H03733"},{"@type":"JGN","@value":"JP15H03733"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H03733/"}],"notation":[{"@language":"ja","@value":"高分解能版大気圏・電離圏モデルによる熱圏重力波の研究"},{"@language":"en","@value":"A study on thermospheric gravity wave using a high resolution atmosphere-ionosphere model"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050296123054925952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Nighttime Midlatitude E-F Coupling in Geomagnetic Conjugate Ionospheres: A Double Thin Shell Model and a Multi-Source Data Investigation"},{"@value":"Nighttime Midlatitude E‐F Coupling in Geomagnetic Conjugate Ionospheres: A Double Thin Shell Model and a Multi‐Source Data Investigation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215432406400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low and Midlatitude Ionospheric Plasma Density Irregularities and Their Effects on Geomagnetic Field"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229802318720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Nonlinear growth, bifurcation, and pinching of equatorial plasma bubble simulated by three‐dimensional high‐resolution bubble model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143950750592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Postsunset vortex in equatorial <i>F</i>‐region plasma drifts and implications for bottomside spread‐<i>F</i>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145449004288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shear flow effects at the onset of equatorial spread <i>F</i>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704780855296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Off‐great‐circle paths in transequatorial propagation: 1. 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