{"_buckets": {"deposit": "68b54fc4-4b67-497a-8530-fd9f346fe757"}, "_deposit": {"created_by": 4, "id": "3644", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "3644"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00003644", "sets": ["528"]}, "author_link": ["4716", "4723", "5276", "3666"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1991-05", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "80", "bibliographicPageStart": "74", "bibliographicVolumeNumber": "4", "bibliographic_titles": [{"bibliographic_title": "Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "OHSHIMA, Kay I.", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "4723", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ONO, Nobuo", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "5276", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "TAKIZAWA, Takatoshi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "4716", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "USHIO, Shuki", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "3666", "nameIdentifierScheme": "WEKO"}]}]}, "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": "Under coastal fast ice in the Ongul Strait near Syowa Station, Antarctica, warmer, more saline, and oxygen-poorer water appears in mid-depth and deep layers from winter to spring every year. This water is explained as a result of mixing between Circumpolar Deep Water (CDW) and Winter Water (WW). This water becomes more like CDW and more homogenized with time from winter to spring, and in December a mixing ratio of 1 : 3-1 : 4 for CDW to WW is required to explain the properties of the homogenized water. It is inferred that the CDW comes along the glacial troughs. Transport of CDW results in a significant amount of heat supply into the water under fast ice.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00003644", "subitem_identifier_reg_type": "JaLC"}]}, "item_1_publisher_22": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "National Institute of Polar Research"}]}, "item_1_source_id_13": {"attribute_name": "雑誌書誌ID", "attribute_value_mlt": [{"subitem_source_identifier": "AA10756213", "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": "Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Institute of Low Temperature Science, Hokkaido University"}, {"subitem_text_language": "en", "subitem_text_value": "Institute of Low Temperature Science, Hokkaido University"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1991-05-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000767847.pdf", "filesize": [{"value": "962.0 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 962000.0, "url": {"label": "KJ00000767847", "url": "https://nipr.repo.nii.ac.jp/record/3644/files/KJ00000767847.pdf"}, "version_id": "c7586b85-f92d-4382-95a4-68472e1fa8bf"}]}, "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": "A NOTE ON WATER EXCHANGE UNDER FAST ICE IN LUTZOW-HOLM BAY, ANTARCTICA", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "A NOTE ON WATER EXCHANGE UNDER FAST ICE IN LUTZOW-HOLM BAY, ANTARCTICA"}]}, "item_type_id": "1", "owner": "4", "path": ["528"], "permalink_uri": "https://doi.org/10.15094/00003644", "pubdate": {"attribute_name": "公開日", "attribute_value": "1991-05-01"}, "publish_date": "1991-05-01", "publish_status": "0", "recid": "3644", "relation": {}, "relation_version_is_last": true, "title": ["A NOTE ON WATER EXCHANGE UNDER FAST ICE IN LUTZOW-HOLM BAY, ANTARCTICA"], "weko_shared_id": 4}