{"_buckets": {"deposit": "f31c4178-84dc-4773-9ba4-68922c57b31c"}, "_deposit": {"id": "5041", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5041"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005041", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2014-10", "bibliographicIssueDateType": "Issued"}, "bibliographicPageStart": "139", "bibliographicVolumeNumber": "66", "bibliographic_titles": [{"bibliographic_title": "Earth, Planets and Space", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Multiple observations of subsurface and surface phenomena during volcanic eruptions provide important information about eruption styles, eruption column dynamics, and magma plumbing systems. During the 2011 eruptions of Kirishima-Shinmoe-dake volcano in Japan, borehole-type tiltmeter data and weather radar data captured the subsurface and surface phenomena, respectively; the tiltmeters detected deflation of a magma chamber caused by migration of magma to the surface, and the weather radar detected changes in the height of the eruption cloud echo. In this study, we present a method based on the correlation between magma chamber deflation and cloud echo height to identify eruption styles. The method can detect whether a column-forming eruption is accompanied by magma migration from the magma chamber (e.g., sub-Plinian eruption), or not (e.g., Vulcanian explosion). By using well-correlated chamber deflation and echo height data, we found that eruption column dynamics during the Shinmoe-dake eruptions are well described by a one-quarter power scaling relationship between cloud height and magma discharge rate, and that a clear correlation between geodetic volume change of the magma chamber and the erupted volume indicates a stable magma plumbing system connecting the magma chamber and the surface.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "SPRINGER HEIDELBERG", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1186/s40623-014-0139-1"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1880-5981", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "T. Kozono", "creatorNameLang": "ja"}, {"creatorName": "T. Kozono", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "H. Ueda", "creatorNameLang": "ja"}, {"creatorName": "H. Ueda", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "T. Shimbori", "creatorNameLang": "ja"}, {"creatorName": "T. Shimbori", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "K. Fukui", "creatorNameLang": "ja"}, {"creatorName": "K. Fukui", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Correlation between magma chamber deflation and eruption cloud height during the 2011 Shinmoe-dake eruptions", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Correlation between magma chamber deflation and eruption cloud height during the 2011 Shinmoe-dake eruptions", "subitem_title_language": "ja"}, {"subitem_title": "Correlation between magma chamber deflation and eruption cloud height during the 2011 Shinmoe-dake eruptions", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5041", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-04-27"}, "publish_date": "2023-04-27", "publish_status": "0", "recid": "5041", "relation": {}, "relation_version_is_last": true, "title": ["Correlation between magma chamber deflation and eruption cloud height during the 2011 Shinmoe-dake eruptions"], "weko_shared_id": -1}