{"@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/1360021390768488192.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/s40623-023-01864-x"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/s40623-023-01864-x.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/s40623-023-01864-x/fulltext.html"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Joint inversion of ocean-bottom pressure and GNSS data from the 2003 Tokachi-oki earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>When the 2003 Tokachi-oki earthquake generated a large tsunami off eastern Hokkaido, Japan, it was detected by cabled ocean-bottom pressure gauges (OBPs) installed within the seismic source region. The OBP records included characteristic features of tsunami waveforms in the source region, indicating significant offset due to the permanent sea-bottom displacement, which can provide critical information about the earthquake source. However, no studies have considered the OBP tsunami data observed in the focal region for the source inversion of the Tokachi-oki earthquake. Here, in order to better understand the 2003 Tokachi-oki earthquake source, we estimate the spatial distribution of fault slip by conducting a joint inversion using two different datasets: tsunami data from four OBPs, located in the focal region and about 300 km away to the south, as well as Global Navigation Satellite System (GNSS) data obtained throughout Hokkaido and northern Honshu. Through our joint inversion, we found that the most dominant slip peak is located 40 km northwest from the hypocenter with an abnormally large slip of <jats:inline-formula><jats:alternatives><jats:tex-math>$$\\sim$$</jats:tex-math><mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\">\n                  <mml:mo>∼</mml:mo>\n                </mml:math></jats:alternatives></jats:inline-formula>15 m. This large slip may result from releasing a high amount of slip deficit accumulated by a stick–slip patch surrounded by stable slip regions on the southernmost Kuril subduction zone. By comparing the OBP observations and the synthetic tsunami waveforms derived from our fault model and other fault models, we conclude that the OBP tsunami data recorded within the focal region better constrained the magnitude and the location of the slip compared to other geophysical data.</jats:p>\n                <jats:p><jats:bold>Graphical Abstract</jats:bold></jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380021390768488192","@type":"Researcher","foaf:name":[{"@value":"SatByul Kim"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390768488196","@type":"Researcher","foaf:name":[{"@value":"Tatsuhiko Saito"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390768488200","@type":"Researcher","foaf:name":[{"@value":"Tatsuya Kubota"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021390768488199","@type":"Researcher","foaf:name":[{"@value":"Sung-Joon Chang"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18805981"}],"prism:publicationName":[{"@value":"Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2023-07-18","prism:volume":"75","prism:number":"1","prism:startingPage":"1"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1186/s40623-023-01864-x.pdf"},{"@id":"https://link.springer.com/article/10.1186/s40623-023-01864-x/fulltext.html"}],"createdAt":"2023-07-18","modifiedAt":"2023-07-18","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=G","dc:title":"G"},{"@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=Ocean-bottom%20pressure%20gauges","dc:title":"Ocean-bottom pressure gauges"},{"@id":"https://cir.nii.ac.jp/all?q=Tsunami","dc:title":"Tsunami"},{"@id":"https://cir.nii.ac.jp/all?q=Joint%20inversion","dc:title":"Joint inversion"},{"@id":"https://cir.nii.ac.jp/all?q=The%202003%20Tokachi-oki%20earthquake","dc:title":"The 2003 Tokachi-oki earthquake"},{"@id":"https://cir.nii.ac.jp/all?q=Geography.%20Anthropology.%20Recreation","dc:title":"Geography. Anthropology. Recreation"},{"@id":"https://cir.nii.ac.jp/all?q=Geodetic%20data","dc:title":"Geodetic data"},{"@id":"https://cir.nii.ac.jp/all?q=Geology","dc:title":"Geology"},{"@id":"https://cir.nii.ac.jp/all?q=Geodesy","dc:title":"Geodesy"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040291932594034944","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22K14126"},{"@type":"JGN","@value":"JP22K14126"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22K14126/"}],"notation":[{"@language":"ja","@value":"直上水圧記録と断層応力解放プロセスから迫る東北沖地震の海溝大すべりメカニズム"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050022708918741504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Frequency dispersion amplifies tsunamis caused by outer-rise normal faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587041605699968","@type":"Article","resourceType":"学術雑誌論文(journal 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Waveform Inversion with Empirical Green's Functions for the 2003 Tokachi-oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865817579023616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source process of the<i>M</i><sub>w</sub>8.3, 2003 Tokachi-Oki, Japan earthquake and its aftershocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865818230990848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Field Survey of the 2003 Tokachi-Oki Earthquake Tsunami and Simulation at the Ootsu Harbor Located at the Pacific Coast of Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518638649856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Offshore geodetic data conducive to the estimation of the afterslip distribution following the 2003 Tokachi-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518943598720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Possibility of recovery of slip deficit rate between the North American plate and the Pacific plate off Sanriku, northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520592809088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Resolving static offsets from high-rate GPS data: the 2003 Tokachi-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694371173476992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tsunami Modeling for the Deep Sea and Inside Focal Areas"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993597332480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Modeling the rupture process of the 2003 September 25 Tokachi‐Oki 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during 1995-2002 estimated from continuous GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945251347968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slip distribution of the 2003 Tokachi‐oki <i>M</i><sub><i>w</i></sub> 8.1 earthquake from joint inversion of tsunami waveforms and geodetic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945412628608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 2003 M8.0 Tokachi‐Oki earthquake – How much has the great event paid back slip debts?"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945438157184","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dispersion and nonlinear effects in the 2011 Tohoku‐Oki earthquake tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419007623040","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tsunami generation by horizontal displacement of ocean bottom"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893538300800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Space time distribution of afterslip following the 2003 Tokachi‐oki earthquake: Implications for variations in fault zone frictional properties"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369148281088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the near-bottom pressure variations in the region of the 2003 Tokachi-Oki tsunami source"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369153892608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Real-time geophysical measurements on the deep seafloor using submarine cable in the southern Kurile subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844440325120","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tsunami waveform inversion incorporating permanent seafloor deformation and its application to tsunami forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319950961664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Micro‐tsunami from a local interplate earthquake detected by cabled offshore tsunami observation in northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794772446720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Recurrence of recent large earthquakes along the southernmost Kurile-Kamchatka Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303610624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Examination of Northeast Edge of the 1952 Tokachi-oki Earthquake Tsunami Source Based on Eyewitness Accounts Stated in Previously Published Reports"},{"@language":"ja","@value":"目撃証言報告に基づく 1952年十勝沖地震の津波波源の北東縁の検討"},{"@language":"ja-Kana","@value":"モクゲキ ショウゲン ホウコク ニ モトズク 1952ネン トカチオキ ジシン ノ ツナミ ハゲン ノ ホクトウエン ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511842048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coseismic and postseismic crustal deformation after the M<SUB>ω</SUB> 8 Tokachi-oki earthquake in Japan"},{"@value":"Coseismic and postseismic crustal deformation after the Mw 8 Tokachi-oki earthquake in Japan"},{"@value":"Post seismic crustal deformation from the Mw 8 Tokachi-oki earthquake on September 26, 2003 in Japan"},{"@value":"Co-seismic and post-seismic crustal deformation after the M8 Tokachi-oki earthquake in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511995520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Compound fault rupture during the 2004 off the Kii Peninsula earthquake (<I>M</I> 7.4) inferred from highly resolved coseismic sea-surface deformation"},{"@value":"Compound fault rupture during the 2004 off the Kii Peninsula earthquake (M 7.4) inferred from highly resolved coseismic sea-surface deformation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512543104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami run-up heights of the 2003 Tokachi-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512545664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The tsunami source area of the 2003 Tokachi-oki earthquake estimated from tsunami travel times and its relationship to the 1952 Tokachi-oki earthquake"},{"@language":"ja-Kana","@value":"tsunami source area of the 2003 Tokachi oki earthquake estimated from tsunami travel times and its relationship to the 1952 Tokachi oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512653312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Re-estimation of tsunami source of the 1952 Tokachi-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512892672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source process of the recurrent Tokachi-oki earthquake on September 26, 2003, inferred from teleseismic body waves"},{"@value":"Source process of the recurrent Tokachi-oki earthquake on September 26, inferred from teleseismic body waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513211264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Joint inversion of strong motion and geodetic data for the source process of the 2003 Tokachi-oki, Hokkaido, earthquake"},{"@value":"Joint inversion of strong motion and geodetic data for the source process of the 2003 Tokachi‐oki, Hokkaido, earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390009224794124288","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2001－2002年に発生した十勝沖の特異な地震活動"},{"@language":"en","@value":"An Unusual Seismic Activity From October, 2001 to June, 2002, off Tokachi, Hokkaido, Japan"},{"@language":"ja-Kana","@value":"2001 2002ネン ニ ハッセイ シタ トカチオキ ノ トクイ ナ ジシン カツドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679282154496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"津波波形から推定した詳細な2003年十勝沖地震のすべり量分布"},{"@language":"en","@value":"Detailed Slip Distribution of the 2003 Tokachi-oki Earthquake Estimated from Tsunami Waveforms"},{"@language":"ja-Kana","@value":"ツナミ ハケイ カラ スイテイ シタ ショウサイ ナ 2003ネン トカチオキ ジシン ノ スベリ リョウ ブンプ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681487883648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inversion of tsunami waveforms for the estimation of a fault heterogeneity: Method and numerical experiments."}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488706176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami source of the 2004 off the Kii Peninsula earthquakes inferred from offshore tsunami and coastal tide gauges"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489199744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Slip distribution of the 2003 Tokachi-oki earthquake estimated from tsunami waveform inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489914368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Ground motion and rupture process of the 2003 Tokachi-oki earthquake obtained from strong motion data of K-NET and KiK-net"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489915520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source rupture process of the 2003 Tokachi-oki earthquake determined by joint inversion of teleseismic body wave and strong ground motion data"},{"@value":"Rupture process of the 2016 Kumamoto earthquake in relation to the thermal structure around Aso 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