{"created":"2023-06-19T11:38:18.433363+00:00","id":5955,"links":{},"metadata":{"_buckets":{"deposit":"0bd0de89-142b-4c58-b127-97082a467154"},"_deposit":{"created_by":13,"id":"5955","owners":[13],"pid":{"revision_id":0,"type":"depid","value":"5955"},"status":"published"},"_oai":{"id":"oai:mie-u.repo.nii.ac.jp:00005955","sets":["420:421:443:472"]},"author_link":["13436"],"item_4_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2004-03-15","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"51","bibliographicPageStart":"25","bibliographicVolumeNumber":"31","bibliographic_titles":[{"bibliographic_title":"三重大学生物資源学部紀要 = The bulletin of the Faculty of Bioresources, Mie University"}]}]},"item_4_description_14":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"渦解像モデルを用いた琉球海流続流に関する数値モデルの結果について,第一部の線形および弱非線形モデルの結果に続いてまとめた。その結果,四国海盆では強い東向流を生じる超非線形型,高気圧渦を生じる非線形型,伊豆海嶺の地形効果で低気圧渦が生じて四国海盆に流入する外部二渦型と四国海盆内部の高気圧が低気圧渦を励起する内部二渦型の4つの流れのパターンが存在することが示された。これらの4つの型の出現はモデルの水深で制御される流れの大きさに依存する。超非線形型の場合には異常に大きい流量を持つ蛇行が生じて,モデルのパラメータ化が現実の海の状況には合わないことが示された。外部二渦型から非線形型へのカオス的な変化が発生し,4つの流れのパターンの中には多重平衡状態の存在が示された。","subitem_description_type":"Abstract"},{"subitem_description":"This paper presents the results of a numerical experiment on a new current, the Ryukyu Current Extension, using the eddy generating model, following the Part I with the models of linear and weak nonlinear ranges. It is shown that four types of current patterns exist in the Shikoku Basin: the Super Nonlinear Pattern with a strong zonal flow, the Nonlinear Pattern with the formation of an anticyclonic eddy, and the External and Internal Two Eddies Patterns with a spin-up and spin-down of the cyclonic eddy. In the External Two-Eddies Pattern, the cyclonic eddy is formed by the topographic effect of the Izu Ridge, but the cyclonic eddy is induced only by the anticyclonic eddy in the Shikoku Basin in the Internal Two Eddies Pattern. Selection of the current pattern depends on the Rossby number, which is controlled by the depth of the model ocean. However, since the Super Nonlinear Pattern with a significantly amplified meander with large volume transport is very different from the observed feature, the model parameter is not suitable for actual oceanic conditions. Results show that a chaotic change from the External Two-Eddies Pattern to the Nonlinear Pattern occurs and a multi-steady state is suggested among these flow patterns.","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"原著論文","subitem_description_type":"Other"}]},"item_4_publisher_30":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"三重大学生物資源学部"}]},"item_4_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0915-0471","subitem_source_identifier_type":"PISSN"}]},"item_4_source_id_9":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN10073846","subitem_source_identifier_type":"NCID"}]},"item_4_text_18":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"A Numerical Experiment on a New Current, the Ryukyu Current Extension, in the Shikoku Basin : Part II Eddy Generating Model"}]},"item_4_text_63":{"attribute_name":"ノート","attribute_value_mlt":[{"subitem_text_value":"NII提供データ"}]},"item_4_text_65":{"attribute_name":"資源タイプ（三重大）","attribute_value_mlt":[{"subitem_text_value":"Departmental Bulletin Paper / 紀要論文"}]},"item_4_version_type_15":{"attribute_name":"著者版フラグ","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":"関根, 義彦","creatorNameLang":"ja"},{"creatorName":"セキネ, ヨシヒコ","creatorNameLang":"ja-Kana"},{"creatorName":"SEKINE, Yoshihiko","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-02-18"}],"displaytype":"detail","filename":"KJ00004095072.pdf","filesize":[{"value":"2.1 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00004095072.pdf","url":"https://mie-u.repo.nii.ac.jp/record/5955/files/KJ00004095072.pdf"},"version_id":"3f7d9e59-db98-4d29-8a59-4ec8e3b6eac5"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Ryukyu Current","subitem_subject_scheme":"Other"},{"subitem_subject":"western boundary current","subitem_subject_scheme":"Other"},{"subitem_subject":"numerical modeling","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"新しい海流である琉球海流続流に関する数値モデル実験 : 第2部 渦解像モデル","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"新しい海流である琉球海流続流に関する数値モデル実験 : 第2部 渦解像モデル","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"13","path":["472"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2007-02-09"},"publish_date":"2007-02-09","publish_status":"0","recid":"5955","relation_version_is_last":true,"title":["新しい海流である琉球海流続流に関する数値モデル実験 : 第2部 渦解像モデル"],"weko_creator_id":"13","weko_shared_id":-1},"updated":"2023-10-13T01:42:43.118278+00:00"}