{"created":"2023-03-31T02:33:57.944057+00:00","id":5521,"links":{},"metadata":{"_buckets":{"deposit":"22feeb3c-3b5d-4f84-b9af-b5f889c8a124"},"_deposit":{"created_by":10,"id":"5521","owners":[10],"pid":{"revision_id":0,"type":"depid","value":"5521"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00005521","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2018","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"49","bibliographicPageStart":"35","bibliographicVolumeNumber":"96A","bibliographic_titles":[{"bibliographic_title":"JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The relationships between the occurrence of intense rainfall and the convergence of surface winds and water vapor concentration for typical heavy-rainfall cases were examined using data from July to August in 2011-2013, obtained from high-density meteorological observations in Tokyo, Japan. Additionally, the temporal variations in wind convergence and water vapor between days with and without heavy rainfall events were compared. Corresponding to heavy-rainfall areas, the convergence of surface winds tended to increase for several tens of minutes prior to the heavy rainfall. The peak of convergence was observed 10-30 min before the heavy-rainfall occurrence, and convergence continued to increase for approximately 30 min until the convergence peak time. Around the heavy-rainfall area, the increase in the water vapor concentration index coincided with the increase in convergence. From these results, by monitoring the temporal variations and distributions of these parameters using a high-density observation network, it should be possible to predict the occurrence of heavy rainfall rapidly and accurately.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"METEOROLOGICAL SOC JAPAN","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.2151/jmsj.2017-020"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"2186-9057","subitem_source_identifier_type":"EISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Yoshihito Seto","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Hitoshi Yokoyama","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Tsuyoshi Nakatani","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Haruo Ando","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Nobumitsu Tsunematsu","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Yoshinori Shoji","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Kenichi Kusunoki","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Masaya Nakayama","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Yuto Saitoh","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Hideo Takahashi","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_title":"Relationships among Rainfall Distribution, Surface Wind, and Precipitable Water Vapor during Heavy Rainfall in Central Tokyo in Summer","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Relationships among Rainfall Distribution, Surface Wind, and Precipitable Water Vapor during Heavy Rainfall in Central Tokyo in Summer","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"10","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2024-06-03"},"publish_date":"2024-06-03","publish_status":"0","recid":"5521","relation_version_is_last":true,"title":["Relationships among Rainfall Distribution, Surface Wind, and Precipitable Water Vapor during Heavy Rainfall in Central Tokyo in Summer"],"weko_creator_id":"10","weko_shared_id":-1},"updated":"2024-06-03T02:00:32.123791+00:00"}