{"@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/1363388844875530880.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/jas3953.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jas/article-pdf/64/7/2502/3619074/jas3953_1.pdf"}}],"dc:title":[{"@value":"Inertia–Gravity Waves Spontaneously Generated by Jets and Fronts. Part I: Different Baroclinic Life Cycles"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>The spontaneous generation of inertia–gravity waves in idealized life cycles of baroclinic instability is investigated using the Weather Research and Forecasting Model. Two substantially different life cycles of baroclinic instability are obtained by varying the initial zonal jet. The wave generation depends strongly on the details of the baroclinic wave’s development. In the life cycle dominated by cyclonic behavior, the most conspicuous gravity waves are excited by the upper-level jet and are broadly consistent with previous simulations of O’Sullivan and Dunkerton. In the life cycle that is dominated by anticyclonic behavior, the most conspicuous gravity waves even in the stratosphere are excited by the surface fronts, although the fronts are no stronger than in the cyclonic life cycle. The anticyclonic life cycle also reveals waves in the lower stratosphere above the upper-level trough of the baroclinic wave; these waves have not been previously identified in idealized simulations. The sensitivities of the different waves to both resolution and dissipation are discussed.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844875530881","@type":"Researcher","foaf:name":[{"@value":"Riwal Plougonven"}],"jpcoar:affiliationName":[{"@value":"School of Mathematics and Statistics, University of St Andrews, St Andrews, United Kingdom"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844875530880","@type":"Researcher","foaf:name":[{"@value":"Chris Snyder"}],"jpcoar:affiliationName":[{"@value":"National Center for Atmospheric Research, Boulder, Colorado"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"15200469"},{"@type":"PISSN","@value":"00224928"}],"prism:publicationName":[{"@value":"Journal of the Atmospheric Sciences"}],"dc:publisher":[{"@value":"American Meteorological Society"}],"prism:publicationDate":"2007-07-01","prism:volume":"64","prism:number":"7","prism:startingPage":"2502","prism:endingPage":"2520"},"reviewed":"false","url":[{"@id":"http://journals.ametsoc.org/jas/article-pdf/64/7/2502/3619074/jas3953_1.pdf"}],"createdAt":"2007-08-01","modifiedAt":"2020-12-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810817767808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A numerical experiment on the formation of the tropopause inversion layer associated with an explosive cyclogenesis: possible role of gravity waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1050568838397612800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quasi-12h inertia-gravity waves in the lower mesosphere observed by the PANSY radar at Syowa Station (39.6°E, 69.0°S)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218811857792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Gravity Wave Characteristics in the Southern Hemisphere Revealed by a High-Resolution Middle-Atmosphere General Circulation Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229804665728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evidence of enhanced double‐diffusive convection below the main stream of the\n                    <scp>K</scp>\n                    uroshio\n                    <scp>E</scp>\n                    xtension"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005519378000640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A study of gravity wave activities based on intensive radiosonde observations at Bengkulu during YMC-Sumatra 2017"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017279830142720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics of Gravity Wave Horizontal Phase Velocity Spectra in the Mesosphere Over the Antarctic Stations, Syowa and Davis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711534826112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Theoretical Study on the Spontaneous Radiation of Inertia–Gravity Waves Using the Renormalization Group Method. Part II: Verification of the Theoretical Equations by Numerical Simulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711534864640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Study of Multiple Tropopause Structures Caused by Inertia–Gravity Waves in the Antarctic"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711536325120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spontaneous Generation of Near-Inertial Waves by the Kuroshio Front"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286989398723584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multiscale Routes to Supply Nutrients Through the Kuroshio Nutrient Stream"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182955623424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cyclone–anticyclone asymmetry in gravity wave radiation from a co-rotating vortex pair in rotating shallow water"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186511536896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Theoretical Study on the Spontaneous Radiation of Inertia–Gravity Waves Using the Renormalization Group Method. 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