{"@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/1362825895112971392.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2009gl038748"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2009GL038748"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2009GL038748"}}],"dc:title":[{"@value":"Surface‐exosphere coupling due to thermal tides"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Using densities measured by accelerometers on the CHAMP and GRACE satellites, and taking advantage of the local time precession characteristics of these near‐polar orbiting satellites, exosphere temperatures are derived as a function of local time, longitude and latitude. Significant longitude variability (e.g., ±25K maximum to minimum over the equator) in geomagnetically‐quiet exosphere temperatures is shown to exist, and is attributed to a spectrum of diurnal and semidiurnal thermal tides that are excited in the troposphere and strongly influenced by the global land‐sea distribution. Since exosphere temperatures are independent of height, this discovery constitutes evidence that exosphere variability is linked to surface variability. Recent evidence suggests that analogous effects exist at Mars.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895112971394","@type":"Researcher","foaf:name":[{"@value":"Jeffrey M. Forbes"}],"jpcoar:affiliationName":[{"@value":"Department of Aerospace Engineering Sciences University of Colorado  Boulder Colorado USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895112971393","@type":"Researcher","foaf:name":[{"@value":"Sean L. Bruinsma"}],"jpcoar:affiliationName":[{"@value":"Department of Terrestrial and Planetary Geodesy Centre Nationale D'Etudes Spatiales  Toulouse France"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895112971395","@type":"Researcher","foaf:name":[{"@value":"Xiaoli Zhang"}],"jpcoar:affiliationName":[{"@value":"Department of Aerospace Engineering Sciences University of Colorado  Boulder Colorado USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895112971392","@type":"Researcher","foaf:name":[{"@value":"Jens Oberheide"}],"jpcoar:affiliationName":[{"@value":"Physics Department University of Wuppertal  Wuppertal Germany"}]}],"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":"2009-08-07","prism:volume":"36","prism:number":"15","prism:startingPage":"L15812"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2009GL038748"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2009GL038748"}],"createdAt":"2009-08-06","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232245199104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Wave-4 structure of the neutral density in the thermosphere and its relation to atmospheric tides"}]},{"@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/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/1390282680297944192","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Theoretical Model of Drag Force Impact on a Model International Space Station Satellite due to Solar Activity"}]},{"@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":"10.1029/2009gl038748"},{"@type":"CROSSREF","@value":"10.1002/2017sw001618_references_DOI_2CKfgNsn03Oy7ZfgJ94umZnMCgk"},{"@type":"CROSSREF","@value":"10.1016/j.jastp.2011.12.002_references_DOI_2CKfgNsn03Oy7ZfgJ94umZnMCgk"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1009-7_references_DOI_2CKfgNsn03Oy7ZfgJ94umZnMCgk"},{"@type":"CROSSREF","@value":"10.2322/tastj.12.47_references_DOI_2CKfgNsn03Oy7ZfgJ94umZnMCgk"},{"@type":"CROSSREF","@value":"10.1016/j.jastp.2010.12.010_references_DOI_2CKfgNsn03Oy7ZfgJ94umZnMCgk"}]}