{"created":"2024-05-17T09:21:52.147251+00:00","id":2005053,"links":{},"metadata":{"_buckets":{"deposit":"1856ec54-8776-4f17-a48b-64de519df372"},"_deposit":{"created_by":10,"id":"2005053","owners":[10],"pid":{"revision_id":0,"type":"depid","value":"2005053"},"status":"published"},"_oai":{"id":"oai:fra.repo.nii.ac.jp:02005053","sets":["12:14:1716951205920"]},"author_link":["3394","3359"],"control_number":"2005053","item_10002_biblio_info_7":{"attribute_name":"bibliographic_information","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1953-10","bibliographicIssueDateType":"Issued"},"bibliographicNumberOfPages":"12","bibliographicPageEnd":"12","bibliographicPageStart":"1","bibliographicVolumeNumber":"5","bibliographic_titles":[{"bibliographic_title":"内海区水産研究所研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"Bulletin of Naikai Regional Fisheries Research Laboratory","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Oceanographical conditions in the Inland Sea region were analysed from the past data. The results were summerrized as follows ; (I. Annual changes of water temperature and salinity in the Inland Sea coincide generally with those of the coastal regions of the Pacific Ocean, but some differences were seen between those at two entrances of the sea as shown in Fig. 3 and Table2. By such differences, the Inland Sea may be divided into two parts. (Fig. 4 and Table 3.) (2). On the standpoint of the influence of offshore water which is distinguished from the smoothness of the annual curves for salinity changes, it is found that the influence from the Bung Suido is of more effective to the Inland Sea than that from the Kii Suido. (3). 4 to 5, 6 and 7 year cycles are found in the long year variations of temperature and salinity in the offshore and the Inland Sea water from the annual mean values and by periodogram analysis of them. (Fig. -5 to 7, and Table 4 to 8)","subitem_description_language":"en","subitem_description_type":"Abstract"},{"subitem_description":"海洋調査要報資料により1923~1944年迄の瀬戸内海及び紀南海域の海況につき論じ,次の諸点を明にした。1)紀南海域は1月~4月にかけて塩分が最大となる。これは黒潮勢力が1月~4月に最強になることを暗示する。2)紀南海域は,累年変化傾向として,4~5年,6年,7年の各周期が認められる。3)瀬戸内海の海況は１カ年の変動性及び,累年変化からみて,紀伊水道より燧灘と,豊後水道より燧灘の2部分に分けられる。4)瀬戸内海の累年変化の傾向として,3年,4~5年,6年の各周期が認められる。","subitem_description_language":"ja","subitem_description_type":"Abstract"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"内海区水産研究所","subitem_publisher_language":"ja"},{"subitem_publisher":"Naikai Regional Fisheries Research Laboratory","subitem_publisher_language":"en"}]},"item_10002_relation_16":{"attribute_name":"情報源","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"nai_k_0501","subitem_relation_type_select":"Local"}}]},"item_10002_relation_17":{"attribute_name":"関連サイト","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_language":"ja","subitem_relation_name_text":"日本農学文献記事索引(agriknowledge)"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://agriknowledge.affrc.go.jp/RN/2010841427","subitem_relation_type_select":"URI"}}]},"item_10002_source_id_11":{"attribute_name":"item_10002_source_id_11","attribute_value_mlt":[{"subitem_source_identifier":"AN00176718","subitem_source_identifier_type":"NCID"}]},"item_10002_source_id_9":{"attribute_name":"item_10002_source_id_9","attribute_value_mlt":[{"subitem_source_identifier":"0497-5022","subitem_source_identifier_type":"PISSN"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Oshima, Yuichi","creatorNameLang":"en","creatorNameType":"Personal"},{"creatorName":"尾島, 雄一","creatorNameLang":"ja","creatorNameType":"Personal"},{"creatorName":"オシマ, ユウイチ","creatorNameLang":"ja-Kana","creatorNameType":"Personal"}],"familyNames":[{"familyName":"Oshima","familyNameLang":"en"},{"familyName":"尾島","familyNameLang":"ja"},{"familyName":"オシマ","familyNameLang":"ja-Kana"}],"givenNames":[{"givenName":"Yuichi","givenNameLang":"en"},{"givenName":"雄一","givenNameLang":"ja"},{"givenName":"ユウイチ","givenNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"3394","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Hisaoka, Minoru","creatorNameLang":"en","creatorNameType":"Personal"},{"creatorName":"久岡, 実","creatorNameLang":"ja","creatorNameType":"Personal"},{"creatorName":"ヒサオカ, ミノル","creatorNameLang":"ja-Kana","creatorNameType":"Personal"}],"familyNames":[{"familyName":"Hisaoka","familyNameLang":"en"},{"familyName":"久岡","familyNameLang":"ja"},{"familyName":"ヒサオカ","familyNameLang":"ja-Kana"}],"givenNames":[{"givenName":"Minoru","givenNameLang":"en"},{"givenName":"実","givenNameLang":"ja"},{"givenName":"ミノル","givenNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"3359","nameIdentifierScheme":"WEKO"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"item_resource_type","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"既往資料による瀬戸内海の海況と漁況の変動　（第１報）海況の周期性について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"既往資料による瀬戸内海の海況と漁況の変動　（第１報）海況の周期性について","subitem_title_language":"ja"},{"subitem_title":"LONG YEAR VARIATIONS OF THE OCEANOGRAPHICAL AND FISHERIES CONDITIONS IN THE INLAND SEA REGION (I). PERIODICITY OF OCEANOGRAPHICAL CONDITIONS","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"10","path":["1716951205920"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2024-05-17"},"publish_date":"2024-05-17","publish_status":"0","recid":"2005053","relation_version_is_last":true,"title":["既往資料による瀬戸内海の海況と漁況の変動　（第１報）海況の周期性について"],"weko_creator_id":"10","weko_shared_id":-1},"updated":"2025-05-26T05:18:21.225839+00:00"}