{"@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/1361699995953170304.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/2008jas2727.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/jas/article-pdf/66/5/1149/3510653/2008jas2727_1.pdf"}}],"dc:title":[{"@value":"Gravity Wave Instability Dynamics at High Reynolds Numbers. Part II: Turbulence Evolution, Structure, and Anisotropy"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>This paper examines the character, intermittency, and anisotropy of turbulence accompanying wave instability, breaking, and turbulence evolution and decay for gravity waves (GW) having a high intrinsic frequency, amplitudes above and below nominal convective instability, and a high Reynolds number. Wave breaking at both amplitudes leads to an extended inertial range of turbulence, with turbulence energies that maximize within ∼1 wave period of the onset of breaking. Turbulence sources include both shear and buoyancy, with shear being the major contributor. Turbulence displays considerable intermittency both within and across the phase of the breaking gravity wave and exhibits clear anisotropy throughout the evolution. Turbulence anisotropy is found at all spatial scales and all times but is most pronounced in the most statically stable phase of the GW and at late times as the turbulent flow restratifies.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995953170305","@type":"Researcher","foaf:name":[{"@value":"David C. Fritts"}],"jpcoar:affiliationName":[{"@value":"NorthWest Research Associates, Colorado Research Associates Division, Boulder, Colorado"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995953170308","@type":"Researcher","foaf:name":[{"@value":"Ling Wang"}],"jpcoar:affiliationName":[{"@value":"NorthWest Research Associates, Colorado Research Associates Division, Boulder, Colorado"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995953170304","@type":"Researcher","foaf:name":[{"@value":"Joe Werne"}],"jpcoar:affiliationName":[{"@value":"NorthWest Research Associates, Colorado Research Associates Division, Boulder, Colorado"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995953170306","@type":"Researcher","foaf:name":[{"@value":"Tom Lund"}],"jpcoar:affiliationName":[{"@value":"NorthWest Research Associates, Colorado Research Associates Division, Boulder, Colorado"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995953170307","@type":"Researcher","foaf:name":[{"@value":"Kam Wan"}],"jpcoar:affiliationName":[{"@value":"NorthWest Research Associates, Colorado Research Associates Division, 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":"2009-05-01","prism:volume":"66","prism:number":"5","prism:startingPage":"1149","prism:endingPage":"1171"},"reviewed":"false","url":[{"@id":"http://journals.ametsoc.org/jas/article-pdf/66/5/1149/3510653/2008jas2727_1.pdf"}],"createdAt":"2008-11-05","modifiedAt":"2020-12-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050862623748258560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simulating turbulent mixing caused by local instability of internal gravity waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711534872832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vertical Wavenumber Spectra of Gravity Waves in the Venus Atmosphere Obtained from Venus Express Radio Occultation Data: Evidence for Saturation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855108883584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical Simulation of Orographic Gravity Waves Observed Over Syowa Station: Wave Propagation and Breaking in the Troposphere and Lower Stratosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1390585658888460544","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"外洋域の鉛直混合に関わる内部波共鳴現象の理論的・数値的研究"},{"@language":"en","@value":"Theoretical and numerical study of internal wave resonance causing vertical mixing in the pelagic ocean"},{"@value":"外洋域の鉛直混合に関わる内部波共鳴現象の理論的・数値的研究 : 2024年度日本海洋学会岡田賞受賞記念論文"},{"@language":"ja-Kana","@value":"ガイヨウイキ ノ エンチョク コンゴウ ニ カカワル ナイブハ キョウメイ ゲンショウ ノ リロンテキ ・ スウチテキ ケンキュウ : 2024ネンド ニホン カイヨウ ガッカイ オカダショウ ジュショウ キネン ロンブン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417166183168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The science case for the EISCAT_3D radar"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1175/2008jas2727.1"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0051-8_references_DOI_BUzNjgGgUoeE0MFmoTwREKZC7GD"},{"@type":"CROSSREF","@value":"10.1017/jfm.2021.119_references_DOI_BUzNjgGgUoeE0MFmoTwREKZC7GD"},{"@type":"CROSSREF","@value":"10.1175/jas-d-14-0315.1_references_DOI_BUzNjgGgUoeE0MFmoTwREKZC7GD"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.34.3_99_references_DOI_BUzNjgGgUoeE0MFmoTwREKZC7GD"},{"@type":"CROSSREF","@value":"10.1029/2023jd039425_references_DOI_1laxgjryiI43DzuNGRGjxSEdrFU"}]}