{"@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/1360004229802359296.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2014ja020878"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2014JA020878"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2014JA020878"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Explicit characteristics of evolutionary‐type plasma bubbles observed from Equatorial Atmosphere Radar during the low to moderate solar activity years 2010–2012"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Using the fan sector backscatter maps of 47 MHz Equatorial Atmosphere Radar (EAR) at Kototabang (0.2°S geographic latitude, 100.3°E geographic longitude, and 10.4°S geomagnetic latitude), Indonesia, the spatial and temporal evolution of equatorial plasma bubbles (EPBs) were examined to classify the evolutionary‐type EPBs from those which formed elsewhere and drifted into the field of view of radar. A total of 535 EPBs were observed during the low to moderate solar activity years 2010–2012, out of which about 210 (~39%) are of evolving type and the remaining 325 (~61%) are drifting‐in EPBs. In general, both the evolving‐type and drifting‐in EPBs exhibit predominance during the postsunset hours of equinoxes and December solstices. Interestingly, a large number of EPBs were found to develop even a few minutes prior to the apex sunset during equinoxes. Further, the occurrence of evolving‐type EPBs exhibits a clear secondary peak around midnight (2300–0100 LT), primarily, due to higher rate of occurrence during the postmidnight hours of June solstices. A significant number (~33%) of postmidnight EPBs generated during June solstices did not exhibited any clear zonal drift, while about 14% of EPBs drifted westward. Also, the westward drifting EPBs are confined only to June solstices. The responsible mechanisms for the genesis of fresh EPBs during postmidnight hours were discussed in light of equatorward meridional winds in the presence of weak westward electric fields.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229802359685","@type":"Researcher","foaf:name":[{"@value":"K. K. Ajith"}],"jpcoar:affiliationName":[{"@value":"Indian Institute of Geomagnetism  Navi Mumbai India"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229802359808","@type":"Researcher","foaf:name":[{"@value":"S. Tulasi Ram"}],"jpcoar:affiliationName":[{"@value":"Indian Institute of Geomagnetism  Navi Mumbai India"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229802359425","@type":"Researcher","foaf:name":[{"@value":"M. Yamamoto"}],"jpcoar:affiliationName":[{"@value":"Research Institute for Sustainable Humanosphere Kyoto University  Uji Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229802359297","@type":"Researcher","foaf:name":[{"@value":"T. Yokoyama"}],"jpcoar:affiliationName":[{"@value":"National Institute of Information and Communications Technology  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229802359556","@type":"Researcher","foaf:name":[{"@value":"V. Sai Gowtam"}],"jpcoar:affiliationName":[{"@value":"Indian Institute of Geomagnetism  Navi Mumbai India"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229802359301","@type":"Researcher","foaf:name":[{"@value":"Y. Otsuka"}],"jpcoar:affiliationName":[{"@value":"Solar Terrestrial Environment Laboratory Nagoya University  Nagoya Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229802359816","@type":"Researcher","foaf:name":[{"@value":"T. Tsugawa"}],"jpcoar:affiliationName":[{"@value":"National Institute of Information and Communications Technology  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229802359302","@type":"Researcher","foaf:name":[{"@value":"K. Niranjan"}],"jpcoar:affiliationName":[{"@value":"Department of Physics Andhra University  Visakhapatnam India"}]}],"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":"2015-02","prism:volume":"120","prism:number":"2","prism:startingPage":"1371","prism:endingPage":"1382"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2014JA020878"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2014JA020878"}],"createdAt":"2015-01-12","modifiedAt":"2023-09-17","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782246988672","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25302007"},{"@type":"JGN","@value":"JP25302007"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25302007/"}],"notation":[{"@language":"ja","@value":"赤道大気レーダーと広域観測網による赤道スプレッドＦ現象と電離圏構造の関連の解明"},{"@language":"en","@value":"Study of relations between Equatorial Spread-F and ionospheric structures with Equatorial Atmosphere Radar and wide-area observation network"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256801950080","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H02135"},{"@type":"JGN","@value":"JP15H02135"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H02135/"}],"notation":[{"@language":"ja","@value":"新・衛星＝地上ビーコン観測と赤道大気レーダーによる低緯度電離圏の時空間変動の解明"},{"@language":"en","@value":"Study of spatio-temporal fluctuation of low latitude ionosphere by using new satellite-ground beacon observation and Equatorial Atmospheric Radar"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810705997952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"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/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/1360001114027745408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Control of the seasonal and longitudinal occurrence of equatorial scintillations by the longitudinal gradient in integrated <i>E</i> region Pedersen conductivity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214348512384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics of large‐scale wave structure observed from African and Southeast Asian longitudinal sectors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214350623616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Climatology of successive equatorial plasma bubbles observed by GPS ROTI over Malaysia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229808199808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vertical rise velocity of equatorial plasma bubbles estimated from Equatorial Atmosphere Radar (EAR) observations and HIRB model simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233290222208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On post‐midnight field‐aligned irregularities observed with a 30.8‐MHz radar at a low latitude: Comparison with<i>F</i>‐layer altitude near the geomagnetic equator"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145357436800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Onset conditions for equatorial spread <i>F</i>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705810723712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Statistical Study of Medium-Scale Traveling Ionospheric Disturbances Observed with a GPS Receiver Network in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708265262720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On postmidnight low-latitude ionospheric irregularities during solar minimum: 2. 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