{"corpus_id":129540724,"paper_sha":"3e51601cba83404f73ba3799e1af51099ed1cf78","doi":"10.1186/s40623-014-0139-1","arxiv_id":null,"pmid":null,"pmcid":null,"mag_id":2125889483,"dblp_id":null,"acl_id":null,"title":"Correlation between magma chamber deflation and eruption cloud height during the 2011 Shinmoe-dake eruptions","year":2014,"publication_date":"2014-10-14","venue":"Earth, Planets and Space","journal":{"name":"Earth, Planets and Space","pages":"1-8","volume":"66"},"journal_issn":null,"journal_title":null,"publication_types":[],"pubmed_pub_types":null,"s2_fields_of_study":["Environmental Science","Geology"],"reference_count":35,"citation_count":14,"influential_citation_count":1,"is_open_access":true,"arxiv_categories":null,"arxiv_license":null,"arxiv_journal_ref":null,"mesh_headings":null,"chemicals":null,"comments_corrections":null,"source_flags":1,"s2_open_access_pdf_url":"https://earth-planets-space.springeropen.com/counter/pdf/10.1186/s40623-014-0139-1","s2_open_access_landing_url":"https://www.semanticscholar.org/paper/3e51601cba83404f73ba3799e1af51099ed1cf78","s2_open_access_license":"CCBY","s2_open_access_status":"GOLD","pmc_open_access_pdf_url":null,"pmc_open_access_landing_url":null,"pmc_open_access_license":null,"pmc_open_access_status":null,"unpaywall_open_access_pdf_url":null,"unpaywall_open_access_landing_url":null,"unpaywall_open_access_license":null,"unpaywall_open_access_status":null,"abstract":"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.","claims":[{"public_id":"cl_ae0f3de086c2a292c28c4a44c2bf9217","status":"active","text":"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 during the 2011 Shinmoe-dake eruptions.","confidence":0.9,"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/claims/cl_ae0f3de086c2a292c28c4a44c2bf9217"},{"public_id":"cl_7281657b9b9732ce65f45a2a50741954","status":"active","text":"A method based on the correlation between magma chamber deflation and cloud echo height can identify eruption styles, distinguishing 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).","confidence":0.95,"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/claims/cl_7281657b9b9732ce65f45a2a50741954"},{"public_id":"cl_818157ce491be248e5e27bc0bb9cf272","status":"active","text":"During the 2011 Shinmoe-dake eruptions, eruption column dynamics are well described by a one-quarter power scaling relationship between cloud height and magma discharge rate.","confidence":0.9,"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/claims/cl_818157ce491be248e5e27bc0bb9cf272"}],"concepts":[{"public_id":"co_3dc0af81cb5057344220238336ff81dd","status":"active","name":"geodetic volume change","description":"Volume change of the magma chamber measured geodetically, correlated with erupted volume during the 2011 Shinmoe-dake eruptions.","types":["measurement"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_3dc0af81cb5057344220238336ff81dd"},{"public_id":"co_48e2aa2374c3336d19dbdf0ba8573908","status":"active","name":"magma chamber deflation","description":"Deflation of a magma chamber detected by borehole-type tiltmeters, caused by migration of magma to the surface during the 2011 Shinmoe-dake eruptions.","types":["phenomenon"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_48e2aa2374c3336d19dbdf0ba8573908"},{"public_id":"co_4be1aa73dfb1dc28d7424eae0f4df24d","status":"active","name":"cloud height","description":"Height of the eruption cloud, used in the one-quarter power scaling relationship with magma discharge rate.","types":["parameter"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_4be1aa73dfb1dc28d7424eae0f4df24d"},{"public_id":"co_56d4d3bbbe64b8335de9d81d85bb76b0","status":"active","name":"eruption styles","description":"Classification of eruptions as column-forming with magma migration (e.g., sub-Plinian) or without (e.g., Vulcanian explosion), identified by correlation of magma chamber deflation and cloud echo height.","types":["classification"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_56d4d3bbbe64b8335de9d81d85bb76b0"},{"public_id":"co_63d0e7e02c62a2d697cacfdaa38bf097","status":"active","name":"cloud echo height","description":"Height of the eruption cloud echo detected by weather radar during the 2011 Shinmoe-dake eruptions.","types":["measurement"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_63d0e7e02c62a2d697cacfdaa38bf097"},{"public_id":"co_7505bc461337f144bf75b3b364e58b2e","status":"active","name":"magma plumbing system","description":"Stable conduit system connecting the magma chamber and the surface, inferred from the correlation between geodetic volume change and erupted volume.","types":["system"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_7505bc461337f144bf75b3b364e58b2e"},{"public_id":"co_84a6c6c0093a9f698b141971d5d94128","status":"active","name":"one-quarter power scaling relationship","description":"A scaling relationship between cloud height and magma discharge rate that describes eruption column dynamics during the 2011 Shinmoe-dake eruptions.","types":["relationship"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_84a6c6c0093a9f698b141971d5d94128"},{"public_id":"co_cd2cd7367c7c0328b421c12890a6369f","status":"active","name":"erupted volume","description":"Volume of material erupted to the surface, correlated with geodetic volume change of the magma chamber.","types":["measurement"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_cd2cd7367c7c0328b421c12890a6369f"},{"public_id":"co_d40beae205412b866b3843eeb72947a9","status":"active","name":"magma discharge rate","description":"Rate of magma discharge from the magma chamber, used in the one-quarter power scaling relationship with cloud height.","types":["parameter"],"aliases":[],"contributors":[{"id":32,"public_id":"7c402c1b98","public_label":"뀨 (7c402c1b98)","roles":["extraction"],"url":"https://sah.borca.ai/u/7c402c1b98"},{"id":17,"public_id":"322360f1c1","public_label":"Killer Whale (322360f1c1)","roles":["review"],"url":"https://sah.borca.ai/u/322360f1c1"},{"id":35,"public_id":"b2adb6bfad","public_label":"Anonymous (b2adb6bfad)","roles":["review"],"url":"https://sah.borca.ai/u/b2adb6bfad"}],"url":"https://sah.borca.ai/concepts/co_d40beae205412b866b3843eeb72947a9"}],"external_ids":{"DOI":"10.1186/s40623-014-0139-1","ArXiv":null,"PubMed":null,"PubMedCentral":null,"MAG":2125889483,"DBLP":null,"ACL":null},"open_access":{"is_open_access":true,"pdf_url":"https://earth-planets-space.springeropen.com/counter/pdf/10.1186/s40623-014-0139-1","landing_url":"https://www.semanticscholar.org/paper/3e51601cba83404f73ba3799e1af51099ed1cf78","source":"semantic_scholar","pdf_url_source":"semantic_scholar_open_access_pdf","license":"CCBY","status":"GOLD","reason":null},"reference_availability":{"status":"available","references_indexed":true,"full_text_available":false,"full_text_source":null,"count_basis":"semantic_scholar_metadata","extraction_status":"not_applicable","reason":null},"source":{"provider":"episteme2","base_corpus":"semantic_scholar_dump","freshness_mode":"unknown","basis":["semantic_scholar_metadata","postgres_metadata"],"limits":["paper metadata is based on indexed upstream scholarly datasets","claims and concepts are available only for extracted papers","absence of claims or concepts means no extracted graph data is available in this response"],"status":"available","degraded":false,"degraded_reasons":[],"diagnostics":{"status":"available","degraded":false,"degraded_reasons":[],"metadata_status":"available","graph_status":"available","abstract_status":"available"},"source_flags":1},"paper_id":635007,"paper_uid":"37156e9f-1bb2-47f3-89ac-5afb8ab4e72f","canonical_identity":{"paper_id":635007,"paper_uid":"37156e9f-1bb2-47f3-89ac-5afb8ab4e72f","identity_status":"available","lookup_basis":"semantic_scholar_external_id","compatibility_path":"corpus_id"},"url":"https://sah.borca.ai/papers/129540724"}