{"@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/1362544418485530752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2008ja013118"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2008JA013118"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008JA013118"}}],"dc:title":[{"@value":"Decay of 3‐m‐scale ionospheric irregularities associated with a plasma bubble observed with the Equatorial Atmosphere Radar"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We investigated the decay processes of 3‐m‐scale ionospheric irregularities associated with plasma bubbles by multi‐instrument observations. The observations were made using the Equatorial Atmosphere Radar (EAR), a 630‐nm airglow imager, and ionosondes. The EAR's electronic beam steering capability allowed us to see the temporal evolution of 3‐m‐scale irregularities associated with plasma bubbles in two‐dimensional views. Around midnight on 28 and 31 March 2006, the EAR detected plasma bubbles that drifted into its field of view. When their eastward drift motion slowed and they finally stopped moving eastward, the 3‐m‐scale irregularities decayed. These results suggest that instability driven by the eastward neutral wind kept the 3‐m‐scale irregularities in matured plasma bubbles, which are in the well‐developed stage, active for several hours after sunset. The stagnated plasma bubbles drifted downward with the ambient westward electric field. This drift resulted in the backscatter echo patterns seen in the range‐time‐intensity (RTI) plots which look like those associated with mid‐latitude plumes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382544418485530755","@type":"Researcher","foaf:name":[{"@value":"Susumu Saito"}],"jpcoar:affiliationName":[{"@value":"Applied Research and Standards Department National Institute of Information and Communications Technology  Koganei, Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544418485530752","@type":"Researcher","foaf:name":[{"@value":"Shoichiro Fukao"}],"jpcoar:affiliationName":[{"@value":"Research Institute for Sustainable Humanosphere Kyoto University  Uji, Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544418485530753","@type":"Researcher","foaf:name":[{"@value":"Mamoru Yamamoto"}],"jpcoar:affiliationName":[{"@value":"Research Institute for Sustainable Humanosphere Kyoto University  Uji, Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544418485530754","@type":"Researcher","foaf:name":[{"@value":"Yuichi Otsuka"}],"jpcoar:affiliationName":[{"@value":"Solar‐Terrestrial Environment Laboratory Nagoya University  Nagoya, Aichi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544418485530756","@type":"Researcher","foaf:name":[{"@value":"Takashi Maruyama"}],"jpcoar:affiliationName":[{"@value":"Applied Research and Standards Department National Institute of Information and Communications Technology  Koganei, Tokyo Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Space Physics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2008-11","prism:volume":"113","prism:number":"A11","prism:startingPage":"n/a"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2008JA013118"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2008JA013118"}],"createdAt":"2008-11-24","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845763736019072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coordinated observations of postmidnight irregularities and thermospheric neutral winds and temperatures at low latitudes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360001114030938880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Continuous generation and two‐dimensional structure of equatorial plasma bubbles observed by high‐density GPS receivers in Southeast Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229806106496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shrinking equatorial plasma bubbles"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021391856319872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A study of equatorial plasma bubble structure using VHF radar and GNSS scintillations over the low-latitude regions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339753512704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First Detection of Midlatitude Plasma Bubble by SuperDARN During a Geomagnetic Storm on May 27 and 28, 2017"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792015355392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geomagnetic conjugacy of plasma bubbles extending to mid-latitudes during a geomagnetic storm on March 1, 2013"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2008ja013118"},{"@type":"OPENAIRE","@value":"doi_dedup___::b8348bf72bb96385dcd763897c30ad60"},{"@type":"CROSSREF","@value":"10.1002/2014ja020433_references_DOI_Iijc0vFv2EYCpZHKEAFNzd7jJKN"},{"@type":"CROSSREF","@value":"10.1002/2016ja022633_references_DOI_Iijc0vFv2EYCpZHKEAFNzd7jJKN"},{"@type":"CROSSREF","@value":"10.1007/s10291-022-01321-4_references_DOI_Iijc0vFv2EYCpZHKEAFNzd7jJKN"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01682-7_references_DOI_Iijc0vFv2EYCpZHKEAFNzd7jJKN"},{"@type":"CROSSREF","@value":"10.1029/2022ja031157_references_DOI_Iijc0vFv2EYCpZHKEAFNzd7jJKN"},{"@type":"CROSSREF","@value":"10.1002/2017ja024048_references_DOI_Iijc0vFv2EYCpZHKEAFNzd7jJKN"}]}