{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282763132437248.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.20965/jdr.2019.p0687"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"029840522"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/029840522"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I029840522"}},{"identifier":{"@type":"URI","@value":"https://www.fujipress.jp/main/wp-content/themes/Fujipress/phyosetsu.php?ppno=DSSTR001400050001"}},{"identifier":{"@type":"NAID","@value":"130007687157"}}],"dc:title":[{"@language":"en","@value":"Tracing Volcanic Activity Chronology from a Multiparameter Dataset at Shinmoedake Volcano (Kirishima), Japan"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>Routine volcano monitoring increasingly involves multiparameter datasets. Databases that include multi-disciplinary datasets have great potential to contribute to the evaluation of ongoing volcanic eruptions and unrest events. Here, we examine the characteristics of a multiparameter dataset from Shinmoedake volcano (Kirishima) in Japan for the period of 2010–2018 to examine how the chronology of volcanic activity can be traced. Our dataset consists of global navigation satellite system (GNSS), seismic, tilt, infrasound, sulfur dioxide (SO<sub>2</sub>) column amount, and video records. We focus mainly on the period after 2012, particularly a series of ash emissions in 2017 (hereafter the 2017 eruption), lava effusion, and Vulcanian eruptions in 2018 (hereafter the 2018 eruption). Our dataset shows that the GNSS observations successfully captured the gradual inflation of the volcano edifice, suggesting magma intrusion or pressure buildup in the magma storage region prior to the 2017 and 2018 eruptions. The number of volcanic earthquakes also gradually increased from 2016 toward the eruptions, particularly events occurring beneath Shinmoedake. Tilt data captured a precursor tilt event prior to the 2017 eruption and a magma chamber deflation during the lava effusion of the 2018 eruption. Tilt, seismic, infrasound, SO<sub>2</sub> gas column, and video data record signals accompanying periodic degassing during the lava effusion and explosive degassing accompanying the Vulcanian eruptions, which have similar characteristics to those reported for past eruptions at Shinmoedake and other volcanoes. This similarity suggests that multidisciplinary databases will be an important reference for future evaluations of ongoing volcanic activity and unrest.</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751153412736","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60804896"},{"@type":"NRID","@value":"1000060804896"},{"@type":"ORCID","@value":"0000-0002-5919-9195"},{"@type":"NRID","@value":"9000400162449"},{"@type":"NRID","@value":"9000375860220"},{"@type":"NRID","@value":"9000380980789"},{"@type":"NRID","@value":"9000347362539"},{"@type":"NRID","@value":"9000375860195"},{"@type":"NRID","@value":"9000403425659"},{"@type":"NRID","@value":"9000404660921"},{"@type":"NRID","@value":"9000380133140"},{"@type":"NRID","@value":"9000375860209"},{"@type":"NRID","@value":"9000402796886"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/taishiyamada"}],"foaf:name":[{"@language":"en","@value":"Yamada Taishi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Research Institute for Earth Science and Disaster Resilience (NIED)"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001204304797959","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000414560808"},{"@type":"NRID","@value":"9000375860088"},{"@type":"NRID","@value":"9000411392522"},{"@type":"NRID","@value":"9000415352473"},{"@type":"NRID","@value":"9000375860231"},{"@type":"NRID","@value":"9000408782781"},{"@type":"NRID","@value":"9000023640625"},{"@type":"NRID","@value":"9000411392268"},{"@type":"NRID","@value":"9000415352913"},{"@type":"NRID","@value":"9000415352767"},{"@type":"NRID","@value":"9000403425660"},{"@type":"NRID","@value":"9000414560840"},{"@type":"NRID","@value":"9000411392515"},{"@type":"NRID","@value":"9000402796885"},{"@type":"NRID","@value":"9000411392711"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/niedueda"}],"foaf:name":[{"@language":"en","@value":"Ueda Hideki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Research Institute for Earth Science and Disaster Resilience (NIED)"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282763132437249","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000403425661"}],"foaf:name":[{"@language":"en","@value":"Mori Toshiya"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geochemical Research Center, Graduate School of Science, The University of Tokyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001204303484801","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000007772153"},{"@type":"NRID","@value":"9000412003020"},{"@type":"NRID","@value":"9000288834198"},{"@type":"NRID","@value":"9000254739965"},{"@type":"NRID","@value":"9000414560809"},{"@type":"NRID","@value":"9000410950107"},{"@type":"NRID","@value":"9000400194271"},{"@type":"NRID","@value":"9000375860087"},{"@type":"NRID","@value":"9000254754130"},{"@type":"NRID","@value":"9000410950074"},{"@type":"NRID","@value":"9000375860232"},{"@type":"NRID","@value":"9000008226565"},{"@type":"NRID","@value":"9000345427405"},{"@type":"NRID","@value":"9000245917958"},{"@type":"NRID","@value":"9000412109042"},{"@type":"NRID","@value":"9000254754004"},{"@type":"NRID","@value":"9000412003046"},{"@type":"NRID","@value":"9000288834477"},{"@type":"NRID","@value":"9000254754191"},{"@type":"NRID","@value":"9000000520398"},{"@type":"NRID","@value":"9000403425662"},{"@type":"NRID","@value":"9000414560839"},{"@type":"NRID","@value":"9000403163616"},{"@type":"NRID","@value":"9000410320054"},{"@type":"NRID","@value":"9000008124447"},{"@type":"NRID","@value":"9000410950091"},{"@type":"NRID","@value":"9000412002563"},{"@type":"NRID","@value":"9000411767621"},{"@type":"NRID","@value":"9000398276583"},{"@type":"NRID","@value":"9000400157958"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0159903"}],"foaf:name":[{"@language":"en","@value":"Tanada Toshikazu"}],"jpcoar:affiliationName":[{"@language":"en","@value":"National Research Institute for Earth Science and Disaster Resilience (NIED)"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"18812473"},{"@type":"EISSN","@value":"18838030"},{"@type":"NDL_BIB_ID","@value":"000008195934"},{"@type":"ISSN","@value":"18812473"},{"@type":"LISSN","@value":"18812473"}],"prism:publicationName":[{"@language":"ja","@value":"Journal of Disaster Research"},{"@language":"en","@value":"Journal of Disaster Research"},{"@language":"en","@value":"J. Disaster Res."}],"dc:publisher":[{"@language":"en","@value":"Fuji Technology Press Ltd."},{"@language":"ja","@value":"富士技術出版株式会社"}],"prism:publicationDate":"2019-08-01","prism:volume":"14","prism:number":"5","prism:startingPage":"687","prism:endingPage":"700"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/029840522"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I029840522"},{"@id":"https://www.fujipress.jp/main/wp-content/themes/Fujipress/phyosetsu.php?ppno=DSSTR001400050001"}],"availableAt":"2019-08-01","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=volcanic%20eruption","dc:title":"volcanic eruption"},{"@id":"https://cir.nii.ac.jp/all?q=database","dc:title":"database"},{"@id":"https://cir.nii.ac.jp/all?q=eruption%20chronology","dc:title":"eruption chronology"},{"@id":"https://cir.nii.ac.jp/all?q=Shinmoedake","dc:title":"Shinmoedake"},{"@id":"https://cir.nii.ac.jp/all?q=Kirishima","dc:title":"Kirishima"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031478354944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Volcanic plume measurements using a UAV for the 2014 Mt. 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to Vulcanian eruptions and gas bursts detected by tilt observations at Semeru Volcano, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691685612288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Monitoring volcanic activity using correlation patterns between infrasound and ground motion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704784673280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relative Source Locations of Continuous Tremor Before and After the Subplinian Events at Shinmoe‐dake, in 2011"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619523343744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"WOVOdat – An online, growing library of worldwide volcanic unrest"}]},{"@id":"https://cir.nii.ac.jp/crid/1360303976321839488","@type":"Article","resourceType":"学術雑誌論文(journal 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Asama, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165869809664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Eruption mass estimation using infrasound waveform inversion and ash and gas measurements: Evaluation at Sakurajima Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182421908864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tephrochronology and eruptive history of Kirishima volcano in southern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095770131840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Strainmeters and tiltmeters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340714499456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reappraisal of volcanic seismicity at the Kirishima 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surveillance"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368436769920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observations of deep long-period (DLP) seismic events beneath Aleutian arc volcanoes; 1989–2002"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845050721792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Similarities and differences in the historical records of lava dome-building volcanoes: Implications for understanding magmatic processes and eruption forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318854523648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Multiparameter quantification of gas release during weak Strombolian eruptions at Pacaya Volcano, Guatemala"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319089972224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Silent fault slip following an interplate thrust earthquake at the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320499473920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An overview of volcano infrasound: From hawaiian to plinian, local to global"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321020509312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Using a process-based model of pre-eruptive seismic patterns to forecast evolving eruptive styles at Sinabung Volcano, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270209408384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subsurface deformations induced by rainfall and atmospheric pressure: tilt/strain measurements in the NE-Italy seismic area"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270458834048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Degassing processes during lava dome growth: Insights from Santiaguito lava dome, Guatemala"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288085239552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"NIED’s V-net, the Fundamental Volcano Observation Network in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679207393280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Volcanism and Crustal Stress Field. Kirishima Volcanoes. Multi active volcanic group generated in a slightly tensile stress field."},{"@value":"特集　火山活動と地殻応力場　霧島　やや張力的応力場に生成した火山群"},{"@language":"ja-Kana","@value":"キリシマ ヤヤ チョウリョクテキ オウリョクバ ニ セイセイシタ カザングン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489147648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A decade of GEONET: 1994-2003"},{"@value":"A decade of GEONET: 1994-2003--The continuous GPS observation in Japan and its impact on earthquake studies"},{"@language":"ja-Kana","@value":"decade of GEONET 1994 2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003 —The continuous GPS observation in Japan and its impact on earthquake studies—"},{"@value":"1994–2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observations in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observation in Japan and its impact on earthquake studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489246592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Precise hypocenter locations of midcrustal low-frequency earthquakes beneath Mt. 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