{"created":"2023-05-15T14:41:40.303539+00:00","id":1626,"links":{},"metadata":{"_buckets":{"deposit":"485a56dc-4746-4067-99d0-8914f898da71"},"_deposit":{"created_by":3,"id":"1626","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"1626"},"status":"published"},"_oai":{"id":"oai:ksu.repo.nii.ac.jp:00001626","sets":["14:13:66"]},"author_link":["4266","4133","7924"],"control_number":"1626","item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2012-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"68","bibliographicPageStart":"43","bibliographicVolumeNumber":"41","bibliographic_titles":[{"bibliographic_title":"京都産業大学論集. 自然科学系列"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"夏季の京都盆地付近における晴天日と雨天日の局地風循環の違いについて，2005年から2007年のデータを利用し，メソ気象領域モデルMM5を用いて解析を行った．京都盆地では，日中に若狭湾や大阪湾の海風，及び琵琶湖起源の湖風によって，収束線が形成され，その領域の上昇流の大きさは，1.0m/sを超えている．収束線の形成場所は，その日の若狭湾や大阪湾起源の海風および琵琶湖起源の湖風の勢力の違いにより異なり，且つ，時間とともに移動している． 京都盆地内に形成される上昇流は，晴天日には上層大気の成層状態が強く，安定しているため， 上昇流が抑えられて，800hPa程度までしか達しない特徴を持つが，雨天日には700hPaを超える範囲まで達する．上昇流の周辺には下降流が形成され，セル状の循環が形成されている．これらのセルの大きさは，京都市市街地付近では大きく，南部の郊外では小さい形状を示していた．また，雨天日の湿数は下層から上層まで小さく，水蒸気を多く含み，雷雨をもたらすような擾乱の指標であるK-indexの値も30を超える大きな値を表していた．このため，雷雨性擾乱の条件が整っており，下層収束が起こることで，より一層雨を伴う驟雨性降水が生じやすい状況であることが確認できた．","subitem_description_type":"Abstract"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"京都産業大学"}]},"item_10002_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA11923897","subitem_source_identifier_type":"NCID"}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1348-3323","subitem_source_identifier_type":"PISSN"}]},"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":"馬場, 賢治","creatorNameLang":"ja"},{"creatorName":"BABA, Kenji","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"4266","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"岡田, 武士","creatorNameLang":"ja"},{"creatorName":"OKADA, Takeshi","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"4133","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"東, 邦昭","creatorNameLang":"ja"},{"creatorName":"HIGASHI, Kuniaki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"7924","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":"2017-09-30"}],"displaytype":"detail","filename":"AHSUSK_NSS_41_43.pdf","filesize":[{"value":"9.5 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breeze","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"K-index","subitem_subject_language":"en","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":"夏季京都盆地周辺における驟雨性降水時の局地風系場の循環について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"夏季京都盆地周辺における驟雨性降水時の局地風系場の循環について","subitem_title_language":"ja"},{"subitem_title":"Local circulation system with heavy rainfall around Kyoto Basin in summer","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"3","path":["66"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2017-09-30"},"publish_date":"2017-09-30","publish_status":"0","recid":"1626","relation_version_is_last":true,"title":["夏季京都盆地周辺における驟雨性降水時の局地風系場の循環について"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-08-09T06:37:28.790512+00:00"}