{"@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/1362825894436097792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2007gl032397"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007GL032397"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GL032397"}}],"dc:title":[{"@value":"Tidal propagation of deep tropical cloud signatures into the thermosphere from TIMED observations"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The diurnal eastward zonal wavenumber‐3 (DE3) tide is excited in the tropical troposphere by latent heat release in deep convective clouds. Its direct propagation into the thermosphere is explored using Hough Mode Extension (HME) analysis of temperature <jats:italic>T</jats:italic>, and zonal and meridional wind (<jats:italic>u</jats:italic>, <jats:italic>v</jats:italic>) measurements from SABER and TIDI on board the TIMED satellite. HMEs provide observation‐based tidal information about parameters not measured (vertical wind <jats:italic>w</jats:italic>, density <jats:italic>ρ</jats:italic>) and at latitudes and altitudes not covered by the two instruments. DE3 in (<jats:italic>u</jats:italic>, <jats:italic>v</jats:italic>, <jats:italic>T</jats:italic>, <jats:italic>ρ</jats:italic>) maximizes around 100 km. The thermospheric (180 km) signal is negligible for (<jats:italic>v</jats:italic>, <jats:italic>ρ</jats:italic>) but still considerable for (<jats:italic>u</jats:italic>, <jats:italic>w</jats:italic>, <jats:italic>T</jats:italic>). Maximum amplitudes are 6 m/s (<jats:italic>u</jats:italic>), 0.12 m/s (<jats:italic>w</jats:italic>), and 8 K (<jats:italic>T</jats:italic>). The HME analysis also shows the quantitative consistency of the DE3 tides from SABER and TIDI in the mesosphere/lower thermosphere region. This allows one to interpret the seasonal DE3 variation in terms of symmetric vs. antisymmetric modes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848661783104134","@type":"Researcher","foaf:name":[{"@value":"J. Oberheide"}],"jpcoar:affiliationName":[{"@value":"Physics Department University of Wuppertal  Wuppertal Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825894436097793","@type":"Researcher","foaf:name":[{"@value":"J. M. Forbes"}],"jpcoar:affiliationName":[{"@value":"Department of Aerospace Engineering Sciences University of Colorado  Boulder Colorado USA"}]}],"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":"2008-02","prism:volume":"35","prism:number":"4","prism:startingPage":"L04816"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007GL032397"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GL032397"}],"createdAt":"2008-02-27","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567183242111744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global response of the ionosphere to atmospheric tides forced from below: Comparison between COSMIC measurements and simulations by atmosphere‐ionosphere coupled model GAIA"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657175346176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Comparison of diurnal tide in models and ground-based observations during the 2005 equinox CAWSES tidal campaign"}]},{"@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"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2007gl032397"},{"@type":"CROSSREF","@value":"10.1029/2011ja017452_references_DOI_TRKC0fTpr8gcMEfTM1DxeFmWSkL"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0832-6_references_DOI_TRKC0fTpr8gcMEfTM1DxeFmWSkL"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1009-7_references_DOI_TRKC0fTpr8gcMEfTM1DxeFmWSkL"},{"@type":"CROSSREF","@value":"10.1016/j.jastp.2010.12.010_references_DOI_TRKC0fTpr8gcMEfTM1DxeFmWSkL"}]}