{"@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/1361137044531484928.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005gl022928"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GL022928"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL022928"}},{"identifier":{"@type":"NAID","@value":"80017814642"}}],"dc:title":[{"@value":"Interannual variability of diurnal tide in the tropical mesopause region: A signature of the El Nino‐Southern Oscillation (ENSO)"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Long‐term MLT radar observations of the diurnal tide at 86 km over Jakarta (6.4°S, 106.7°E) and Tirunelveli (8.7°N, 77.8°E) during the years 1993–1999 are examined in this work. Monthly estimates of tidal amplitudes in the meridional direction over these sites reveal a pronounced interannual variability. The satellite derived Outgoing Longwave Radiation (OLR) is used as a proxy for deep tropical convection in this study. Removal of composite seasonal cycle yields ‘anomalies’ in the diurnal tide over Jakarta and Tirunelveli that are correlated with the OLR anomalies over the western Pacific region (∼120°E). It is suggested that the lower atmospheric large‐scale convective systems originating over the western Pacific region in response to the El Nino Southern Oscillation (ENSO) facilitate excitation of nonmigrating tides through latent heat release or large‐scale redistribution of water vapor that compete with the dominant migrating tide and possibly induce the observed interannual variability in the diurnal tide.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1583387451286768384","@type":"Researcher","foaf:name":[{"@value":"S. Gurubaran"}],"jpcoar:affiliationName":[{"@value":"Equatorial Geophysical Research Laboratory Indian Institute of Geomagnetism Tirunelveli India"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016867239582210","@type":"Researcher","foaf:name":[{"@value":"R. Rajaram"}],"jpcoar:affiliationName":[{"@value":"Equatorial Geophysical Research Laboratory Indian Institute of Geomagnetism Tirunelveli India"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016867239582208","@type":"Researcher","foaf:name":[{"@value":"T. Nakamura"}],"jpcoar:affiliationName":[{"@value":"Research Institute for Sustainable Humanosphere Kyoto University Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016867239582209","@type":"Researcher","foaf:name":[{"@value":"T. Tsuda"}],"jpcoar:affiliationName":[{"@value":"Research Institute for Sustainable Humanosphere Kyoto University Kyoto Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2005-07","prism:volume":"32","prism:number":"13","prism:startingPage":"L13805"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005GL022928"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005GL022928"}],"createdAt":"2005-07-05","modifiedAt":"2024-01-27","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360017282426722304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Impact of Tropospheric Ozone Modulation Due To El Niño on Tides in the MLT"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704784839424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"ENSO effects on MLT diurnal tides: A 21 year reanalysis data‐driven GAIA model simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179762665600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The non–storm time corrugated upper thermosphere: What is beyond MSIS?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183245356928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial Features of L‐Band Equinoctial Scintillations From Equator to Low Midlatitude at Around 95°E During 2015–2016"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849946528448640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"100 Years of Progress in Understanding the Stratosphere and Mesosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503107584","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Gravity Wave Characteristics over the Equator Observed During the CPEA Campaign using Simultaneous Data from Multiple Stations"},{"@value":"Gravity Wave Characteristics over the Equator Observed During the CPEA Campaign using Simultaneous Data from Multiple Stations(<Special Issue>CPEA-Coupling Processes in the Equatorial Atmosphere)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681479787008","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coupling Processes in the Equatorial Atmosphere (CPEA): A Project Overview"},{"@value":"Coupling Processes in the Equatorial Atmosphere (CPEA) : A Project Overview(<Special Issue>CPEA-Coupling Processes in the Equatorial Atmosphere)"}]},{"@id":"https://cir.nii.ac.jp/crid/1520010380533240704","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Radar observations of the diurnal tide in the tropical mesosphere-lower thermosphere region: longitudinal variabilities"},{"@language":"ja-Kana","@value":"Radar observations of the diurnal tide in the tropical mesosphere lower thermosphere region longitudinal variabilities"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290884467964544","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"赤道大気上下結合"},{"@language":"ja-Kana","@value":"セキドウ タイキ ジョウゲ ケツゴウ"},{"@language":"ja","@value":"4.赤道大気上下結合(2005年度秋季大会シンポジウム「大規模観測プロジェクトは気象学に何をもたらすか」の報告)"},{"@language":"en","@value":"Coupling Processes in the Equatorial Atmospherer (CPEA)(What Do BIG Observation Projects Bring to Us? : A Report on the Symposium of the 2005 Fall Assembly of the Meteorological Society of Japan)"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892082788736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"El Nino–Southern Oscillation effect on quasi-biennial oscillations of temperature diurnal tides in the mesosphere and lower thermosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892090761344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"El Niño–Southern Oscillation efect on ionospheric tidal/SPW amplitude in 2007– 2015 FORMOSAT-3/COSMIC observations"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892145980800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermospheric inter-annual variability and its potential connection to ENSO and stratospheric QBO"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005gl022928"},{"@type":"CIA","@value":"80017814642"},{"@type":"OPENAIRE","@value":"doi_dedup___::eb61dc33325de473b28ae76dcf01447d"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0455-8_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.1029/2023gl102790_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.1002/2017ja024011_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.1002/2017sw001618_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.1029/2018ja025533_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.2151/jmsj.84a.1_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0832-6_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1009-7_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.1175/amsmonographs-d-19-0003.1_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"},{"@type":"CROSSREF","@value":"10.2151/jmsj.84a.239_references_DOI_5vxKbj5OCk5pemlqKk5zVMzTV3l"}]}