{"created":"2023-06-20T13:42:38.070733+00:00","id":173,"links":{},"metadata":{"_buckets":{"deposit":"6afa8c4e-b4ea-4cb9-8db7-8bcc96f68cf4"},"_deposit":{"created_by":2,"id":"173","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"173"},"status":"published"},"_oai":{"id":"oai:fut.repo.nii.ac.jp:00000173","sets":["1"]},"author_link":["9043","9042"],"item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2003-03-20","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"33","bibliographicPageEnd":"237","bibliographicPageStart":"231","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":"Surface boundary layer has important role for water and energy exchange between atmosphere and land surface. The transportation process of water and energy in the surface boundary layer affects the local and regional hydrlo-meteorological environment. The author has observed micro meteorological phenomena in the layer at Awara campus of Fukui University of Technology since 2000. In this paper the author reports the observation results, especially surface energy budget and evaporation in 2002. Latent heat flux amounts to 90% of net radiation. The amount of evaporation from January to September is estimated to be about 800mm. These values may be slightly overestimated","subitem_description_type":"Abstract"}]},"item_10002_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.57375/00000167","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":"TF00008626","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":"9042","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Ujihashi, Yasuyuki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"9043","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":"KJ00004279706.pdf","filesize":[{"value":"666.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00004279706.pdf","url":"https://fut.repo.nii.ac.jp/record/173/files/KJ00004279706.pdf"},"version_id":"3450b1d1-7e89-41f2-ae60-24492f428765"}]},"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":"芦原北潟湖畔における地表面熱収支特性","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"芦原北潟湖畔における地表面熱収支特性"},{"subitem_title":"Surface energy budget at Awara near the Lake Kitagata","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":"173","relation_version_is_last":true,"title":["芦原北潟湖畔における地表面熱収支特性"],"weko_creator_id":"2","weko_shared_id":-1},"updated":"2023-06-20T14:38:20.385121+00:00"}