{"@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/1361137045540667264.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/qj.377"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.377"}},{"identifier":{"@type":"URI","@value":"https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.377"}}],"dc:title":[{"@value":"A framework for testing global non‐hydrostatic models"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>With the emergence of non‐hydrostatic global dynamical cores, an alternative testing strategy is proposed, where the planetary radius is suitably reduced to capture non‐hydrostatic phenomena without incurring the computational cost of actual simulations of weather and climate at non‐hydrostatic resolution. The procedure is simple and tests various aspects of the discretized hydrostatic and non‐hydrostatic equations in the same setting on a sphere. Furthermore, it facilitates verification against Cartesian‐domain analytic solutions and against large‐eddy simulation (LES) benchmarks available for limited‐area models. The proposed framework is illustrated with examples of inertia–gravity wave dynamics in linear and nonlinear regimes, including flows past idealized mountains, stratified shear flows and critical layers. Finally, an intercomparison of the Held–Suarez climate variability for reduced‐size planets is presented, which provides a path for future investigations on the dynamics of convective boundary layers on a sphere. This assesses the ability to adequately capture interactions of large‐scale dynamics with intermittent turbulent structures, an important aspect of future weather and climate predictions. Copyright © 2009 Royal Meteorological Society</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137045540667264","@type":"Researcher","foaf:name":[{"@value":"Nils P. Wedi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045540667265","@type":"Researcher","foaf:name":[{"@value":"Piotr K. Smolarkiewicz"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00359009"},{"@type":"EISSN","@value":"1477870X"}],"prism:publicationName":[{"@value":"Quarterly Journal of the Royal Meteorological Society"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2009-01","prism:volume":"135","prism:number":"639","prism:startingPage":"469","prism:endingPage":"484"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.377"},{"@id":"https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.377"}],"createdAt":"2009-02-19","modifiedAt":"2023-10-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285715172782976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global 7-km mesh nonhydrostatic Model Intercomparison Project for improving TYphoon forecast (TYMIP-G7): Experimental design and preliminary results"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380154635776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Convection-Permitting Climate Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694594881717120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"DCMIP2016: the splitting supercell test case"}]},{"@id":"https://cir.nii.ac.jp/crid/1390003825190660608","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Global Simulations of the Atmosphere at 1.45 km Grid-Spacing with the Integrated Forecasting System"},{"@language":"ja","@value":"Integrated Forecasting System による 1.45km水平格子間隔での大気の全球シミュレーション"},{"@value":"Special Edition on DYAMOND : The DYnamics of the Atmospheric general circulation Modeled On Non-hydrostatic Domains : Global Simulations of the Atmosphere at 1.45 km Grid-Spacing with the Integrated Forecasting System"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842089639168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Non-hydrostatic Icosahedral Atmospheric Model : description and development"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/qj.377"},{"@type":"CROSSREF","@value":"10.1186/s40645-014-0018-1_references_DOI_RAIlEjQ0CDkFLU9zRdH9hW16qZ5"},{"@type":"CROSSREF","@value":"10.2151/jmsj.2020-016_references_DOI_RAIlEjQ0CDkFLU9zRdH9hW16qZ5"},{"@type":"CROSSREF","@value":"10.5194/gmd-10-1363-2017_references_DOI_RAIlEjQ0CDkFLU9zRdH9hW16qZ5"},{"@type":"CROSSREF","@value":"10.1016/b978-0-323-96026-7.00194-6_references_DOI_RAIlEjQ0CDkFLU9zRdH9hW16qZ5"},{"@type":"CROSSREF","@value":"10.5194/gmd-12-879-2019_references_DOI_RAIlEjQ0CDkFLU9zRdH9hW16qZ5"}]}