{"created":"2023-07-25T11:00:27.981367+00:00","id":2293,"links":{},"metadata":{"_buckets":{"deposit":"b5f6926a-d13e-470b-ae76-914519d376c3"},"_deposit":{"created_by":4,"id":"2293","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2293"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002293","sets":["1:356:405"]},"author_link":["1862","59027","59025","59023","59028","59024","59026"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1996-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"315","bibliographicPageStart":"307","bibliographicVolumeNumber":"51","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Special issue"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Jones,E. P.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Aagaard,K.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Carmack,E. C.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Macdonald,R. W.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Mclaughlin,F. A.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Perkin,R. G.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Swift J. H.","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"A comparison of historical oceanographic data from the Arctic Ocean with that obtained aboard the CCGS Louis s. St. Laurent during the Canada/U.S. 1994 Arctic Ocean Section unequivocally shows that the mid-depth layers of the Arctic Ocean are experiencing a major warming and ventilation event. The intrusion of new water is characterized by (a) higher values in the Atlantic Layer maximum temperatures, (b) a shallower core depth for the temperature maximum, (c) displacement of waters of Pacific origin in the upper 100-200m, and (d) pronounced thermohaline inversions 40-60m thick in the Atlantic Layer and Upper Deep waters. The largest temperature change, as much as 1℃, is seen in the core of the Atlantic Layer, suggesting that the event is related to an increase in the transport and/or temperature of water entering from the North Atlantic.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733561","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Department of Fisheries and Oceans, Bedford Institute of Oceanography/Polar Science Center, Applied Physics Laboratory, University of Washington/Department of Fisheries and Oceans, Institute of Ocean Sciences/Department of Fisheries and Oceans, Institute of Ocean Sciences/Department of Fisheries and Oceans, Institute of Ocean Sciences/Department of Fisheries and Oceans, Institute of Ocean Sciences/Scripps Institution of Oceanography"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1996-12-01"}],"displaytype":"detail","filename":"KJ00000012845.pdf","filesize":[{"value":"1.0 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000012845","url":"https://nipr.repo.nii.ac.jp/record/2293/files/KJ00000012845.pdf"},"version_id":"6b0e92de-5e63-49f4-8d1c-ca40f4561c56"}]},"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":"Recent changes in Arctic Ocean thermohaline structure: Results from the Canada/U.S. 1994 Arctic Ocean section (scientific paper)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Recent changes in Arctic Ocean thermohaline structure: Results from the Canada/U.S. 1994 Arctic Ocean section (scientific paper)","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["405"],"pubdate":{"attribute_name":"公開日","attribute_value":"1996-12-01"},"publish_date":"1996-12-01","publish_status":"0","recid":"2293","relation_version_is_last":true,"title":["Recent changes in Arctic Ocean thermohaline structure: Results from the Canada/U.S. 1994 Arctic Ocean section (scientific paper)"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T13:46:31.337481+00:00"}