{"created":"2023-07-25T08:05:54.996296+00:00","id":4507,"links":{},"metadata":{"_buckets":{"deposit":"a8778026-f878-47b5-bfe6-0742c45f4c4d"},"_deposit":{"created_by":18,"id":"4507","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"4507"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00004507","sets":["228:262:4853","39:40"]},"author_link":["101789"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1956-01-30","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"19","bibliographicPageStart":"12","bibliographicVolumeNumber":"4","bibliographic_titles":[{"bibliographic_title":"鹿児島大学水産学部紀要","bibliographic_titleLang":"ja"},{"bibliographic_title":"Memoirs of Faculty of Fisheries Kagoshima University","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1956-01-30","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"We made some researches on harmonic analysis of water temperature  ascertained as the results of the monthly regular observations from the surface to the depth of 200m layer in Kagoshima Bay during the lapse of twelve  months. The following results were obtained. As to the mean water temperature of the whole year, in the limited  depth from the surface to 75m layer, it showed the highest degree at the mouth of Bay (Sec. I) and the lowest at the northern region (Sec.  V)  . But in  100m layer or in the layer deeper than that, it hardly showed any variation in spite of the difference in each section of the layer. \nThe variance of the surface water temperature was found to be largest in the northern section of the Bay. As to the amplitudes for annual changes of the surface water temperature, they were larger in the northern section than in any other, and at the layer from  10-100m they were largest at the mouth of the Bay. The water masses both in the 75m and deeper layer of sec. V and in the 100m and deeper layer at the south of Sakurazima were hardly influenced by the land water and the oceanic water. As to the phase angles it was confirmed that the time lag for the maximum and minimum temperature during the whole year increased gradually as the depth became deeper and the section shifted to the northern region.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0453087X","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00040498","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"660","subitem_subject_scheme":"NDC"}]},"item_7_subject_20":{"attribute_name":"NIIsubject","attribute_value_mlt":[{"subitem_subject":"自然科学","subitem_subject_language":"ja","subitem_subject_scheme":"Other"}]},"item_7_version_type_14":{"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":"田ノ上, 豊隆","creatorNameLang":"ja"},{"creatorName":"TANOUE, Toyotaka","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"101789","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":"2016-10-27"}],"displaytype":"detail","filename":"無題3.pdf","filesize":[{"value":"784.5 kB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"無題3.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/4507/files/無題3.pdf"},"version_id":"59d00859-0c98-4f1d-9c5a-4ae1a1b88d24"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"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":"鹿児島灣に於ける水温の年変化の調和分析","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"鹿児島灣に於ける水温の年変化の調和分析","subitem_title_language":"ja"},{"subitem_title":"The Harmonic Analysis of Annual Variation of Water Temperature in Kagoshima Bay","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["40","4853"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2011-03-16"},"publish_date":"2011-03-16","publish_status":"0","recid":"4507","relation_version_is_last":true,"title":["鹿児島灣に於ける水温の年変化の調和分析"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-07-30T01:15:01.965041+00:00"}