{"created":"2023-03-31T02:31:03.841223+00:00","id":5432,"links":{},"metadata":{"_buckets":{"deposit":"5ed73178-c617-4741-9734-c5e34b268066"},"_deposit":{"id":"5432","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"5432"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00005432","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2016-02-01","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"30","bibliographicPageStart":"15","bibliographicVolumeNumber":"11","bibliographic_titles":[{"bibliographic_title":"Journal of Disaster Research","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Preliminary results of quantitative analysis of volcanic ash clouds observed over the Sakurajima volcano in Kagoshima, Japan, were obtained by using weather radar and surface instruments. The Ka-band Doppler radar observations showed the inner structure of a volcanic ash column every two minutes after an eruption. Operational X-band polarimetric radar provides information on three-dimensional ash fall amount distribution. The terminal fall velocity of ash particles was studied by using optical disdrometers, together with the main specifications of observation instruments.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Fuji Technology Press Ltd.","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.20965/jdr.2016.p0015"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1883-8030","subitem_source_identifier_type":"EISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"M. Maki","creatorNameLang":"ja"},{"creatorName":"M. Maki","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"M. Iguchi","creatorNameLang":"ja"},{"creatorName":"M. Iguchi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"T. Maesaka","creatorNameLang":"ja"},{"creatorName":"T. Maesaka","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"T. Miwa","creatorNameLang":"ja"},{"creatorName":"T. Miwa","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"T. Tanada","creatorNameLang":"ja"},{"creatorName":"T. Tanada","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"T. Kozono","creatorNameLang":"ja"},{"creatorName":"T. Kozono","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"T. Momotani","creatorNameLang":"ja"},{"creatorName":"T. Momotani","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"A. Yamaji","creatorNameLang":"ja"},{"creatorName":"A. Yamaji","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"I. Kakimoto","creatorNameLang":"ja"},{"creatorName":"I. Kakimoto","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_title":"Preliminary Results of Weather Radar Observations of Sakurajima Volcanic Smoke","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Preliminary Results of Weather Radar Observations of Sakurajima Volcanic Smoke","subitem_title_language":"ja"},{"subitem_title":"Preliminary Results of Weather Radar Observations of Sakurajima Volcanic Smoke","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"1","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-04-27"},"publish_date":"2023-04-27","publish_status":"0","recid":"5432","relation_version_is_last":true,"title":["Preliminary Results of Weather Radar Observations of Sakurajima Volcanic Smoke"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-04-27T05:18:33.282514+00:00"}