{"created":"2023-07-25T09:03:09.153299+00:00","id":763,"links":{},"metadata":{"_buckets":{"deposit":"30974c04-bdfb-48a4-b77c-568a38ca2939"},"_deposit":{"created_by":3,"id":"763","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"763"},"status":"published"},"_oai":{"id":"oai:toyama.repo.nii.ac.jp:00000763","sets":["74:77:133:142"]},"author_link":["131496","131497"],"item_3_alternative_title_19":{"attribute_name":"その他（別言語等）のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Large-scale temperature rise in the Japanese Islands and its generation factor"}]},"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2010-11","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"99","bibliographicPageStart":"83","bibliographicVolumeNumber":"5","bibliographic_titles":[{"bibliographic_title":"富山大学人間発達科学部紀要"}]}]},"item_3_description_15":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"In this study, the large-scale temperature rise in the Japanese Islands was taken up. The daily values of AMeDAS in 2004 were used for data. Large-scale temperature rise was defined as the case when the deviation from the normal of the daily maximum temperature is 10℃ or more. First of all, the region and the season of large-scale temperature rise were clarified. Then, the generation was analyzed. The results are as follows.\n1) Large-scale temperature rise occurs mainly in the Sea of Japan coast from San-in to Tohoku. A lot of generations are also seen in Pacific coast and the Okhotsk coast from Kanto to Hokkaido. Many appear in spring.\n2) Large-scale temperature rise starts from West Japan, and shifts to East Japan. Moreover, it starts from the inland, and shifts to the coast. Before and after the generation of a large-scale temperature rise, the anticyclone advances toward the east around Japanese Islands. When the Japanese Islands are covered with the anticyclone, warm air is formed in the inland. The warm air is carried to the leeward coast by the southerly wind on the west side of the anticyclone. This wind blocks the invasion of a cool sea breeze, and promotes the temperature rise.","subitem_description_type":"Abstract"}]},"item_3_description_40":{"attribute_name":"資源タイプ(DSpace)","attribute_value_mlt":[{"subitem_description":"Article","subitem_description_type":"Other"}]},"item_3_description_6":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"富山大学人間発達科学部紀要, 5巻1号, Page 83-99","subitem_description_type":"Other"}]},"item_3_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"131497","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Tagami, Yoshio"}]}]},"item_3_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15099/00000757","subitem_identifier_reg_type":"JaLC"}]},"item_3_publisher_33":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"富山大学人間発達科学部"}]},"item_3_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA12181167","subitem_source_identifier_type":"NCID"}]},"item_3_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1881316X","subitem_source_identifier_type":"ISSN"}]},"item_3_version_type_16":{"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":"田上, 善夫"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-02-15"}],"displaytype":"detail","filename":"01-07_5-1_83-99_2010_ver2.pdf","filesize":[{"value":"5.3 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"01-07_5-1_83-99_2010_ver2.pdf","url":"https://toyama.repo.nii.ac.jp/record/763/files/01-07_5-1_83-99_2010_ver2.pdf"},"version_id":"e92852d9-46c0-4952-ade1-49e31de5974d"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"昇温","subitem_subject_scheme":"Other"},{"subitem_subject":"フェーン","subitem_subject_scheme":"Other"},{"subitem_subject":"暖気","subitem_subject_scheme":"Other"},{"subitem_subject":"強風","subitem_subject_scheme":"Other"},{"subitem_subject":"temperature rise","subitem_subject_scheme":"Other"},{"subitem_subject":"foehn","subitem_subject_scheme":"Other"},{"subitem_subject":"warm air","subitem_subject_scheme":"Other"},{"subitem_subject":"strong wind","subitem_subject_scheme":"Other"}]},"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":"日本列島における大規模昇温とその発生要因","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"日本列島における大規模昇温とその発生要因"}]},"item_type_id":"3","owner":"3","path":["142"],"pubdate":{"attribute_name":"公開日","attribute_value":"2011-01-31"},"publish_date":"2011-01-31","publish_status":"0","recid":"763","relation_version_is_last":true,"title":["日本列島における大規模昇温とその発生要因"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-07-25T15:26:43.044539+00:00"}