{"@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/1363670318375785472.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2000gl003744"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000GL003744"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000GL003744"}}],"dc:title":[{"@value":"Terdiurnal oscillations in OH Meinel rotational temperatures for fall conditions at northern mid‐latitude sites"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>High‐precision (∼0.5 K) measurements of OH Meinel (M) (6,2) rotational temperatures above the Bear Lake Observatory, UT (42°N, 112°W) during October 1996 have revealed an interesting and unexpected mean nocturnal pattern. Ten quality nights (>100 h) of data have been used to form a mean night for autumnal, near‐equinoctial conditions. The mean temperature and RMS variability associated with this mean night were 203 ± 5 K and 2.4 K, respectively, and compare very favorably with expectations based on Na‐lidar measurements of mean tidal temperature perturbations over Urbana, IL (40°N, 88°W) during the fall 1996. Furthermore, this comparison shows that the 8‐h tide was the dominant source of the mean nocturnal temperature variability in the OH M region during this period. Additional data, obtained at Fort Collins, CO (41°N, 105°W) in November 1997, illustrate the occurrence of an 8‐h component of OH temperature variability about two months after the equinox and show that daily amplitudes as high as ≅15 K are possible.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318375785345","@type":"Researcher","foaf:name":[{"@value":"W. R. Pendleton"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318375785344","@type":"Researcher","foaf:name":[{"@value":"M. J. Taylor"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318375785346","@type":"Researcher","foaf:name":[{"@value":"L. C. Gardner"}]}],"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":"2000-06-15","prism:volume":"27","prism:number":"12","prism:startingPage":"1799","prism:endingPage":"1802"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000GL003744"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000GL003744"}],"createdAt":"2002-09-17","modifiedAt":"2023-11-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050570852905480832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temporal evolutions of N2+Meinel (1,2) band near 1.5.mu m associated with aurora breakup and their effects on mesopause temperature estimations from OH Meinel (3,1) band"},{"@value":"Temporal evolutions of N+2 Meinel (1,2) band near 1.5.μm associated with aurora breakup and their effects on mesopause temperature estimations from OH Meinel (3,1) band"},{"@value":"Temporal evolutions of $$\\text {N}_2^+$$ Meinel (1,2) band near $$1.5.\\,\\upmu \\text {m}$$ associated with aurora breakup and their effects on mesopause temperature estimations from OH Meinel (3,1) band"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658217661696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the occurrence and variability of the terdiurnal tide in the equatorial mesosphere and lower thermosphere and a comparison with the Kyushu-GCM"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2000gl003744"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01360-0_references_DOI_TMze3w9qgIjzEoTJSFGn8onsn6P"},{"@type":"CROSSREF","@value":"10.1029/2010jd014529_references_DOI_TMze3w9qgIjzEoTJSFGn8onsn6P"}]}