{"@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/2051151842060084352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/s40623-021-01522-0"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/digimeta/12287052"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/12287052"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/s40623-021-01522-0.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/s40623-021-01522-0/fulltext.html"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Crisis hazard assessment for snow-related lahars from an unforeseen new vent eruption : the 2018 eruption of Kusatsu-Shirane volcano, Japan"}],"dcterms:alternative":[{"@value":"Crisis hazard assessment for snow-related lahars from an unforeseen new vent eruption : the 2018 eruption of Kusatsu-Shirane volcano, Japan"}],"dc:language":"en","description":[{"notation":[{"@value":"収集根拠 : オンライン資料収集制度"},{"@value":"資料形態 : テキストデータ"},{"@value":"コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/2061151842060084352","@type":"Researcher","foaf:name":[{"@value":"Kyoko S. Kataoka"}]},{"@id":"https://cir.nii.ac.jp/crid/2061151842060084353","@type":"Researcher","foaf:name":[{"@value":"Kae Tsunematsu"}]},{"@id":"https://cir.nii.ac.jp/crid/2061151842060084354","@type":"Researcher","foaf:name":[{"@value":"Takane Matsumoto"}]}],"publication":{"publicationIdentifier":[{"@type":"ISSN","@value":"18805981"},{"@type":"LISSN","@value":"13438832"},{"@type":"EISSN","@value":"18805981"}],"prism:publicationName":[{"@value":"EPS : Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Nature"}],"prism:publicationDate":"2021-12-11","prism:volume":"73(220)","prism:startingPage":"220"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/digimeta/12287052"},{"@id":"https://dl.ndl.go.jp/pid/12287052"},{"@id":"https://link.springer.com/content/pdf/10.1186/s40623-021-01522-0.pdf"},{"@id":"https://link.springer.com/article/10.1186/s40623-021-01522-0/fulltext.html"}],"foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=QB275-343","dc:title":"QB275-343"},{"@id":"https://cir.nii.ac.jp/all?q=QE1-996.5","dc:title":"QE1-996.5"},{"@id":"https://cir.nii.ac.jp/all?q=Snow%20survey","dc:title":"Snow survey"},{"@id":"https://cir.nii.ac.jp/all?q=Crisis%20hazard%20map","dc:title":"Crisis hazard map"},{"@id":"https://cir.nii.ac.jp/all?q=Geology","dc:title":"Geology"},{"@id":"https://cir.nii.ac.jp/all?q=Flow%20simulation","dc:title":"Flow simulation"},{"@id":"https://cir.nii.ac.jp/all?q=Titan2D","dc:title":"Titan2D"},{"@id":"https://cir.nii.ac.jp/all?q=G","dc:title":"G"},{"@id":"https://cir.nii.ac.jp/all?q=Lahar","dc:title":"Lahar"},{"@id":"https://cir.nii.ac.jp/all?q=Geography.%20Anthropology.%20Recreation","dc:title":"Geography. Anthropology. Recreation"},{"@id":"https://cir.nii.ac.jp/all?q=Geodesy","dc:title":"Geodesy"},{"@id":"https://cir.nii.ac.jp/all?q=Snow-clad%20volcano","dc:title":"Snow-clad volcano"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256969292032","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"18H01291"},{"@type":"JGN","@value":"JP18H01291"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18H01291/"}],"notation":[{"@language":"ja","@value":"隠された小規模噴火と火山泥流の高時間分解能履歴解明:噴火頻度と災害範囲の再評価"},{"@language":"en","@value":"Unraveling small-scale eruptions and lahar events by high-resolution stratigraphy of distally deposited volcaniclastic deposits: Re-assessment of eruption frequency and hazard risk areas"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050287142172520448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Locating hydrothermal fluid injection of the 2018 phreatic eruption at Kusatsu-Shirane volcano with volcanic tremor amplitude"}]},{"@id":"https://cir.nii.ac.jp/crid/1050568617200406400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Anatomy of active volcanic edifice at the Kusatsu–Shirane volcano, Japan, by magnetotellurics: hydrothermal implications for volcanic unrests"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845763137851776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lahar characteristics as a function of triggering mechanism at a seasonally snow-clad volcano: contrasting lahars following the 2014 phreatic eruption of Ontake Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050852870543559424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 2018 phreatic eruption at Mt. Motoshirane of Kusatsu–Shirane volcano, Japan: Eruption and intrusion of hydrothermal fluid observed by a borehole tiltmeter network"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005744245266688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Time Variation in the Chemical and Isotopic Composition of Fumarolic Gasses at Kusatsu-Shirane Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145569992832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hyperconcentrated flow — transitional process between water flow and debris flow"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146171199360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Perturbation and melting of snow and ice by the 13 November 1985 eruption of Nevado del Ruiz, Colombia, and consequent mobilization, flow and deposition of lahars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146211419648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluating Titan2D mass-flow model using the 1963 Little Tahoma Peak avalanches, Mount Rainier, Washington"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013172689875456","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hazards at Ice-Clad Volcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013173015194496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of Titan2D modelling forecasts for the 2007 Crater Lake break-out lahar, Mt. Ruapehu, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013173039117440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slushflow hazard — where, why and when? 25 years of experience with slushflow consulting and research"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707927307904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Observations and numerical simulations of the braking effect of forests on large-scale avalanches"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619342066816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A study of the Taisho lahar generated by the 1926 eruption of Tokachidake Volcano, central Hokkaido, Japan, and implications for the generation of cohesive lahars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294646502118144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Secondary lahar hazard assessment for Villa la Angostura, Argentina, using Two-Phase-Titan modelling code during 2011 Cordón Caulle eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294646754661888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hydrologic consequences of hot-rock/snowpack interactions at Mount St. Helens Volcano, Washington"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294646849919232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"How do the grain size characteristics of a tephra deposit change over time?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294646860940416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evaluation of the Titan2D two-phase flow model using an actual event: Case study of the 2005 Vazcún Valley Lahar"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647548724224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lahars at Cotopaxi and Tungurahua Volcanoes, Ecuador"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647840308480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flow behavior of channelized debris flows, Mount St. Helens, Washington"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568470777535104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"From sink to volcanic source: Unravelling missing terrestrial eruption records by characterization and high‐resolution chronology of lacustrine volcanic density flow deposits, Lake Inawashiro‐ko, Fukushima, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576121542336768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ablation of debris‐covered ice: some effects of the 25 September 2007 Mt Ruapehu eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576122761462144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An empirical method for estimating travel times for wet volcanic mass flows"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232159398272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A kitchen experiment for replicating lava-ice interaction on stratovolcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569002363520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Objective delineation of lahar-inundation hazard zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570957331584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A two-fluid model for avalanche and debris flows"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857596729383040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lahars of Cotopaxi Volcano, Ecuador: hazard and risk evaluation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707394378880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"From ‘source to sink’ to ‘sink to source’: a review of volcanic fluvial and lacustrine successions in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043702652928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tephra, snow and water: complex sedimentary responses at an active snow-capped stratovolcano, Ruapehu, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046428876672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volcanic mixed avalanches: A distinct eruption-triggered mass-flow process at snow-clad volcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993434003840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentology, Behavior, and Hazards of Debris Flows at Mount Rainier, Washington"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994500850048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Water, ice and mud: lahars and lahar hazards at ice‐ and snow‐clad volcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995354389632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fluid Mechanical Description of Fluidized Beds. Equations of Motion"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943707692928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Osceola Mudflow from Mount Rainier: Sedimentology and hazard implications of a huge clay-rich debris flow"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946379723264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Integrating multidisciplinary science, modelling and impact data into evolving, syn-event volcanic hazard mapping and communication: A case study from the 2012 Tongariro eruption crisis, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894754533632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeling lahar behavior and hazards"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895506480896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Explaining the extreme mobility of volcanic ice-slurry flows, Ruapehu volcano, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896161469184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 25 September 2007 eruption of Mount Ruapehu, New Zealand: Directed ballistics, surtseyan jets, and ice-slurry lahars"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370312504448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Parallel adaptive numerical simulation of dry avalanches over natural terrain"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318596058240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Computing granular avalanches and landslides"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319372657152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The motion of a finite mass of granular material down a rough incline"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793561017856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rain-on-snow induced flood events in Southern Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268887867264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lahar hazard assessment using Titan2D for an alluvial fan with rapidly changing geomorphology: Whangaehu River, Mt. Ruapehu"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269554497408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The surface energy balance of an active ice-covered volcano: Villarrica Volcano, southern Chile"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237167360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"草津白根火山の地質"},{"@language":"en","@value":"Geology of Kusatsu-Shirane Volcano"},{"@language":"ja-Kana","@value":"クサツ シラネ カザン ノ チシツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513720064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Two electrical conductors beneath Kusatsu-Shirane volcano, Japan, imaged by audiomagnetotellurics, and their implications for the hydrothermal system"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282752367848832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Accumulation and ablation of seasonal snow cover around Azuma and Adatara Volcanoes"},{"@language":"ja","@value":"吾妻・安達太良火山周辺地域における積雪の堆積・消耗特性"}]},{"@id":"https://cir.nii.ac.jp/crid/1390582783486892928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Principal component analysis for the elemental composition of sedimentary sands in the Hayakawa River of Hakone Caldera, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845712971122816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Kusatsu-Shirane volcano as a site of phreatic eruptions"},{"@language":"ja","@value":"水蒸気噴火発生場としての草津白根火山"},{"@language":"ja-Kana","@value":"スイジョウキ フンカ ハッセイジョウ ト シテ ノ クサツ シロネ カザン"}]},{"@id":"https://cir.nii.ac.jp/crid/1391131406289827968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology and eruption history of the Motoshirane Pyroclastic Cone Group, Kusatsu-Shirane Volcano, central Japan"},{"@language":"ja","@value":"草津白根火山，本白根火砕丘群の地質と形成史"},{"@language":"ja-Kana","@value":"クサツ シロネ カザン,ホン シロネ カサイキュウグン ノ チシツ ト ケイセイシ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892104451456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Total mass estimate of the January 23, 2018, phreatic eruption of Kusatsu-Shirane Volcano, central Japan"}]}],"dataSourceIdentifier":[{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R100000039-I12287052"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01522-0"},{"@type":"KAKEN","@value":"PRODUCT-23846096"},{"@type":"OPENAIRE","@value":"doi_dedup___::5368a36f4b5aec826cdf3ecfd8e7b39c"},{"@type":"CROSSREF","@value":"10.3389/feart.2023.1116157_references_DOI_Z6Y0vuIwMGkEj893wirCJjtrHgk"},{"@type":"CROSSREF","@value":"10.2343/geochemj.gj24013_references_DOI_Z6Y0vuIwMGkEj893wirCJjtrHgk"},{"@type":"CROSSREF","@value":"10.1144/sp520-2022-171_references_DOI_Z6Y0vuIwMGkEj893wirCJjtrHgk"}]}