{"created":"2023-05-15T14:41:39.147062+00:00","id":1599,"links":{},"metadata":{"_buckets":{"deposit":"fa207ab2-7fde-45fd-9d0f-e8521fd993b1"},"_deposit":{"created_by":3,"id":"1599","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"1599"},"status":"published"},"_oai":{"id":"oai:ksu.repo.nii.ac.jp:00001599","sets":["14:13:62"]},"author_link":["7924","18474"],"control_number":"1599","item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2008-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"93","bibliographicPageStart":"81","bibliographicVolumeNumber":"37","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":"1999年の1年間に京阪神を通過した寒冷前線を地上天気図から22例を検出した．これらについて気象庁現業用レーダーの降水エコーなどを調べた結果，3時間に100mm以上の大雨をもたらした顕著な線状降水帯が3例（5月27日，6月27日，6月29日）確認できた．本研究は，どのような環境場のときに，これらの線状降水帯が形成されたのかについて調べることが目的である．まず，潮岬の高層気象観測データによると，線状降水帯の事例では対流圏下層においてほぼ南西の風が卓越し，風速は20m/s を上回っていた．さらに，潮岬の高層観測データから925hPaの水蒸気フラックスと対流有効位置エネルギーを算出した．これによると，線状降水帯が発現した場合には水蒸気フラックスが350g/m^2·sを上回っていることがわかった．また，対流有効位置エネルギーと水蒸気フラックスの関係を調べると，水蒸気フラックスの値が同じ位の値であれば，対流有効位置エネルギーが大きい場合に線状降水帯が発生しており，一方，対流有効位置エネルギーが同じ位の値であれば，水蒸気フラックスの値が大きい場合に線状降水帯が発生していることが明らかになった．","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":"東, 邦昭","creatorNameLang":"ja"},{"creatorName":"HIGASHI, Kuniaki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"藤井, 健","creatorNameLang":"ja"},{"creatorName":"FUJII, Takeshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"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_37_81.pdf","filesize":[{"value":"547.3 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"AHSUSK_NSS_37_81.pdf","url":"https://ksu.repo.nii.ac.jp/record/1599/files/AHSUSK_NSS_37_81.pdf"},"version_id":"d330f002-6ab2-42ef-a7a6-daaedee918c8"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"線状降水帯","subitem_subject_scheme":"Other"},{"subitem_subject":"寒冷前線","subitem_subject_scheme":"Other"},{"subitem_subject":"風向風速場","subitem_subject_scheme":"Other"},{"subitem_subject":"水蒸気フラックス","subitem_subject_scheme":"Other"},{"subitem_subject":"対流有効位置エネルギー","subitem_subject_scheme":"Other"},{"subitem_subject":"Line-shaped precipitation system","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"cold front","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"wind field","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"water vapor flux","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"convective available potential energy","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":"1999年に京阪神地域を通過した寒冷前線に伴って線状降水帯が発生したときの環境場","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"1999年に京阪神地域を通過した寒冷前線に伴って線状降水帯が発生したときの環境場","subitem_title_language":"ja"},{"subitem_title":"Environmental Characteristics to Formation of Line-shaped Precipitation Systems in Passing of Cold Fronts in the Keihanshin Area in 1999","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"3","path":["62"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2017-09-30"},"publish_date":"2017-09-30","publish_status":"0","recid":"1599","relation_version_is_last":true,"title":["1999年に京阪神地域を通過した寒冷前線に伴って線状降水帯が発生したときの環境場"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-08-22T00:57:13.307938+00:00"}