{"@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/1363670320379295104.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/ja088ia06p04869"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJA088iA06p04869"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JA088iA06p04869"}}],"dc:title":[{"@value":"On the generation and growth of equatorial backscatter plumes: 2. Structuring of the west walls of upwellings"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The west wall of large‐scale ‘upwellings’ that develop in the bottomside of the nighttime equatorial <jats:italic>F</jats:italic> layer becomes structured by the wind‐driven gradient drift instability, the same process that leads to the formation of striations in barium ion clouds. Upwellings are initiated by wavelike perturbations with long spatial wavelengths (∼400‐km) and are amplified by the collisional Rayleigh‐Taylor instability (and sometimes assisted by the gradient drift instability in the case of an upward moving <jats:italic>F</jats:italic> layer). The west wall structuring process is driven by an eastward neutral wind enhanced by reduced drag during the postsunset hours and a velocity shear in east‐west bulk plasma drift in the bottomside <jats:italic>F</jats:italic> layer. West wall structures evolve in a manner analogous to primary plasma bubbles, i.e., secondary plasma bubbles grow from the west wall. Their characteristics are compared with those of the primary bubbles and discussed in the light of existing theories.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320379295104","@type":"Researcher","foaf:name":[{"@value":"Roland T. Tsunoda"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Space Physics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1983-06","prism:volume":"88","prism:number":"A6","prism:startingPage":"4869","prism:endingPage":"4874"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJA088iA06p04869"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JA088iA06p04869"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810705997952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On the application of differential phase measurements to study the zonal large scale wave structure (LSWS) in the ionospheric electron content"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229804174208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"West wall structuring of equatorial plasma bubbles simulated by three‐dimensional HIRB model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232245213312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On validating the relationship of ionogram signatures to large-scale wave structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017279830097664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multi‐Event Analysis of Magnetosphere‐Ionosphere Coupling of Nighttime Medium‐Scale Traveling Ionospheric Disturbances From the Ground and the Arase Satellite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390558288768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling of Multi‐Ion Plasma Bubbles in the Equatorial Ionosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360282588962526080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First observations of large‐scale wave structure and equatorial spread F using CERTO radio beacon on the C/NOFS satellite"}]},{"@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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