{"created":"2023-03-31T02:37:57.221529+00:00","id":5653,"links":{},"metadata":{"_buckets":{"deposit":"ec1534a9-a8e6-48da-a5a9-c60f5c471d95"},"_deposit":{"id":"5653","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"5653"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00005653","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2005","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"49","bibliographicPageEnd":"30","bibliographicPageStart":"25","bibliographicVolumeNumber":"49","bibliographic_titles":[{"bibliographic_title":"水工学論文集","bibliographic_titleLang":"ja"},{"bibliographic_title":"PROCEEDINGS OF HYDRAULIC ENGINEERING","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"This paper describes relationships between Niño 3 sea water temperature (SST) and statistical characteristics of daily rainfalls in Tokyo. Daily rainfall series for 1961-2002 is separated the series in the years with positive SST-anomalies from the one in the years with negative SST-anomalies. The frequency analysis based on partial duration series is carried out individually. The quantiles in the years with negative SST-anomalies are 1.68-2.35 times as large as the ones in the years with the positive SST-anomalies, indicating that the heavy rainfall events occur frequently in the years with negative SST-anomalies. Despite the condition of no artificial factor in the climate changes such as a global warming, the numerical simulation results using the ocean-atmosphere coupled general circulation model also show that the daily rainfall series in Tokyo is unstationary.","subitem_description_language":"ja","subitem_description_type":"Other"},{"subitem_description":"This paper describes relationships between Niño 3 sea water temperature (SST) and statistical characteristics of daily rainfalls in Tokyo. Daily rainfall series for 1961-2002 is separated the series in the years with positive SST-anomalies from the one in the years with negative SST-anomalies. The frequency analysis based on partial duration series is carried out individually. The quantiles in the years with negative SST-anomalies are 1.68-2.35 times as large as the ones in the years with the positive SST-anomalies, indicating that the heavy rainfall events occur frequently in the years with negative SST-anomalies. Despite the condition of no artificial factor in the climate changes such as a global warming, the numerical simulation results using the ocean-atmosphere coupled general circulation model also show that the daily rainfall series in Tokyo is unstationary.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"公益社団法人 土木学会","subitem_publisher_language":"ja"},{"subitem_publisher":"Japan Society of Civil Engineers","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.2208/prohe.49.25"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0916-7374","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"東 博紀","creatorNameLang":"ja"},{"creatorName":"HIGASHI Hironori","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"飯塚 聡","creatorNameLang":"ja"},{"creatorName":"IIZUKA Satoshi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"松浦 知徳","creatorNameLang":"ja"},{"creatorName":"MATSUURA Tomonori","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_title":"Nino3海域の海面水温変動と東京における豪雨発生","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Nino3海域の海面水温変動と東京における豪雨発生","subitem_title_language":"ja"},{"subitem_title":"RELATIONSHIPS BETWEEN NIÑO 3 SEA SURFACE TEMPERATURE AND STATISTICAL CHARACTERISTICS OF HEAVY RAINFALLS IN TOKYO","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"1","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-03-30"},"publish_date":"2023-03-30","publish_status":"0","recid":"5653","relation_version_is_last":true,"title":["Nino3海域の海面水温変動と東京における豪雨発生"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-08T09:27:35.599378+00:00"}