{"created":"2023-05-15T12:35:40.109120+00:00","id":4671,"links":{},"metadata":{"_buckets":{"deposit":"083cece7-5a8f-4238-a590-6c95a25aca84"},"_deposit":{"created_by":91,"id":"4671","owners":[91],"pid":{"revision_id":0,"type":"depid","value":"4671"},"status":"published"},"_oai":{"id":"oai:nitech.repo.nii.ac.jp:00004671","sets":["31"]},"author_link":["8782","8782","14842"],"item_10001_biblio_info_28":{"attribute_name":"bibliographic_information","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1999-02","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"377","bibliographicPageStart":"368","bibliographicVolumeNumber":"11","bibliographic_titles":[{"bibliographic_title":"PHYSICS OF FLUIDS","bibliographic_titleLang":"en"}]}]},"item_10001_description_36":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"The mechanism of heat transport in geostrophic flows under various density stratifications has been studied by using both direct numerical simulation and rapid distortion theory. It is found that in cases with rotation, the iso-surfaces of the temperature fluctuations are aligned in the direction of the rotational axis, and they become very close to two-dimensional. Under stable stratification with rotation, the velocity and temperature fluctuations tend to oscillate with the Brunt-Vaisala frequency, while they tend to oscillate with a longer period in cases without rotation. Under unstable stratification with rotation, on the other hand, vortex columns are formed in the direction parallel to the axis of rotation owing to the effects of nonlinear interactions.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_full_name_27":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"8782","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000070273307","nameIdentifierScheme":"NRID","nameIdentifierURI":"http://rns.nii.ac.jp/nr/1000070273307"}],"names":[{"name":"飯田, 雄章"}]}]},"item_10001_publisher_29":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"American Institute of Physics","subitem_publisher_language":"en"}]},"item_10001_source_id_30":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1070-6631","subitem_source_identifier_type":"ISSN"}]},"item_10001_source_id_32":{"attribute_name":"item_10001_source_id_32","attribute_value_mlt":[{"subitem_source_identifier":"AA10986203","subitem_source_identifier_type":"NCID"}]},"item_10001_version_type_33":{"attribute_name":"出版タイプ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Iida, Oaki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"8782","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000070273307","nameIdentifierScheme":"NRID","nameIdentifierURI":"http://rns.nii.ac.jp/nr/1000070273307"}]},{"creatorNames":[{"creatorName":"Nagano, Y.","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"14842","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-01-24"}],"displaytype":"detail","filename":"POF 11_368.pdf","filesize":[{"value":"1.4 MB"}],"format":"application/pdf","license_note":"Copyright (1999) American Institute of Physics. This article may be downloaded for personal use only. Any other use requires prior permission of the author and the American Institute of Physics.The following article appeared in Physics of Fluids, 11(2), pp.368- 377 ; 1999 and may be found at http://link.aip.org/link/?phf/11/368","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"本文_fulltext","url":"https://nitech.repo.nii.ac.jp/record/4671/files/POF 11_368.pdf"},"version_id":"49e2159f-717c-4202-aafc-4b9df783b71c"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"item_resource_type","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Coherent  structure and heat transfer in geostrophic flow under density stratification","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Coherent  structure and heat transfer in geostrophic flow under density stratification","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"91","path":["31"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2012-11-06"},"publish_date":"2012-11-06","publish_status":"0","recid":"4671","relation_version_is_last":true,"title":["Coherent  structure and heat transfer in geostrophic flow under density stratification"],"weko_creator_id":"91","weko_shared_id":-1},"updated":"2025-03-17T04:16:18.825524+00:00"}