{"created":"2023-06-20T13:42:40.815738+00:00","id":236,"links":{},"metadata":{"_buckets":{"deposit":"d06cb207-0e57-44fc-9870-fe2dacf94a0c"},"_deposit":{"created_by":2,"id":"236","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"236"},"status":"published"},"_oai":{"id":"oai:fut.repo.nii.ac.jp:00000236","sets":["1"]},"author_link":["9267","9266"],"item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2007-05-31","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"37","bibliographicPageEnd":"212","bibliographicPageStart":"205","bibliographic_titles":[{"bibliographic_title":"福井工業大学研究紀要. 第一部"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Bowen ratio method is one of the popular methods for flux measurement. The meteorological conditions and /or the assumptions to apply the method are not necessary satisfied at some observation sites. Therefore, the estimated latent and sensible heat fluxes do not agree with each other when measurement heights differ, and sometimes it is not easy to estimate fluxes accurately. In this paper, the author conducted the experiment to observe the evaporation from ground surface at near the Lake Kitagata, Awara City. Comparing estimated and observed evaporation, it shows that evaporation rates can be estimated within plus or minus 10 to 20% by using the data measured at 2m and 4m.","subitem_description_type":"Abstract"}]},"item_10002_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.57375/00000230","subitem_identifier_reg_type":"JaLC"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"福井工業大学"}]},"item_10002_relation_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"TF00008689","subitem_relation_type_select":"NCID"}}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"2868571","subitem_source_identifier_type":"ISSN"}]},"item_10002_version_type_20":{"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":"宇治橋, 康行"}],"nameIdentifiers":[{"nameIdentifier":"9266","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Ujihashi, Yasuyuki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"9267","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":"2023-04-12"}],"displaytype":"detail","filename":"KJ00004766965.pdf","filesize":[{"value":"740.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00004766965.pdf","url":"https://fut.repo.nii.ac.jp/record/236/files/KJ00004766965.pdf"},"version_id":"4d211e39-bebc-4246-b046-00f820acfdfa"}]},"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":"芦原北潟湖周辺における地表面熱・水収支特性に関する研究","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"芦原北潟湖周辺における地表面熱・水収支特性に関する研究"},{"subitem_title":"Energy and water balance at near the lake Kitagata, Awara City Fukui Prefecture","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"2","path":["1"],"pubdate":{"attribute_name":"公開日","attribute_value":"2009-04-04"},"publish_date":"2009-04-04","publish_status":"0","recid":"236","relation_version_is_last":true,"title":["芦原北潟湖周辺における地表面熱・水収支特性に関する研究"],"weko_creator_id":"2","weko_shared_id":-1},"updated":"2023-06-20T14:36:48.651665+00:00"}