{"@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/1360848658222291968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018jb015832"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB015832"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015832"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB015832"}},{"identifier":{"@type":"URI","@value":"http://api.wiley.com/onlinelibrary/chorus/v1/articles/10.1029%2F2018JB015832"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015832"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Using Tsunami Waves Reflected at the Coast to Improve Offshore Earthquake Source Parameters: Application to the 2016 Mw 7.1 Te Araroa Earthquake, New Zealand"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The Te Araroa earthquake occurred on 2 September 2016 (local time) offshore of the northeastern coast of New Zealand's North Island (Mw 7.1). When this event occurred, ocean bottom pressure gauges (OBPs), installed ~170 km south of the source area, clearly recorded direct tsunami from the source to OBPs (~ −1.5 cm), and tsunami from coastal reflections (~2 cm). We estimate the centroid location that best reproduces the OBP waveforms. When using the direct wave alone, the centroid location is poorly constrained, with a horizontal uncertainty of ~100 km. By combining both direct and reflected tsunami waveforms, we obtain a centroid location near the Global Centroid Moment Tensor centroid (~80 km northeast from the coast) with smaller uncertainty (~40 km). We also estimate the earthquake source dimension (length and width) and found that the models using coastal reflections require a source dimension larger than ~30 km long. Based on the slip distribution obtained by the finite fault inversion, we obtain an energy‐based stress drop Δ<jats:italic>σ</jats:italic><jats:sub>E</jats:sub>of 1.0 MPa, consistent with typical earthquake stress drop values. This study shows that the information added by coastal reflected tsunami provides much tighter constraints on the centroid location, source dimension, and stress drop of offshore earthquakes, which is difficult to obtain from the onshore seismic data alone. Future studies should utilize the information provided by coastal reflected waves to improve earthquake source modeling using ocean bottom pressure data.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848658222291985","@type":"Researcher","foaf:name":[{"@value":"Tatsuya Kubota"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848658222291855","@type":"Researcher","foaf:name":[{"@value":"Tatsuhiko Saito"}],"jpcoar:affiliationName":[{"@value":"National Research Institute for Earth Science and Disaster Resilience Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276172946176","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30435581"},{"@type":"NRID","@value":"1000030435581"},{"@type":"ORCID","@value":"0000-0001-9484-9539"},{"@type":"CINII_AUTHOR_ID","@value":"DA17240097"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA17240097#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA17240097"},{"@type":"NRID","@value":"9000002327811"},{"@type":"NRID","@value":"9000254263259"},{"@type":"NRID","@value":"9000254741331"},{"@type":"NRID","@value":"9000001755219"},{"@type":"NRID","@value":"9000001756269"},{"@type":"NRID","@value":"9000413695854"},{"@type":"NRID","@value":"9000254263251"},{"@type":"NRID","@value":"9000412206699"},{"@type":"NRID","@value":"9000283726644"},{"@type":"NRID","@value":"9000258283045"},{"@type":"NRID","@value":"9000380434917"},{"@type":"NRID","@value":"9000410949101"},{"@type":"NRID","@value":"9000016847657"},{"@type":"NRID","@value":"9000347135736"},{"@type":"NRID","@value":"9000391404808"},{"@type":"NRID","@value":"9000347166246"},{"@type":"NRID","@value":"9000006894368"},{"@type":"NRID","@value":"9000347135626"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0134551"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/YoshihiroIto"}],"foaf:name":[{"@value":"Yoshihiro Ito"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute Kyoto University Uji Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848658222291850","@type":"Researcher","foaf:name":[{"@value":"Yoshihiro Kaneko"}],"jpcoar:affiliationName":[{"@value":"GNS Science Lower Hutt New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848658222291860","@type":"Researcher","foaf:name":[{"@value":"Laura M. Wallace"}],"jpcoar:affiliationName":[{"@value":"GNS Science Lower Hutt New Zealand"},{"@value":"Institute for Geophysics University of Texas at Austin Austin TX USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848658222291852","@type":"Researcher","foaf:name":[{"@value":"Syuichi Suzuki"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Science Tohoku University Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848658222291972","@type":"Researcher","foaf:name":[{"@value":"Ryota Hino"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Science Tohoku University Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848658222291714","@type":"Researcher","foaf:name":[{"@value":"Stuart Henrys"}],"jpcoar:affiliationName":[{"@value":"GNS Science Lower Hutt New Zealand"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2018-10","prism:volume":"123","prism:number":"10","prism:startingPage":"8767","prism:endingPage":"8779"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018JB015832"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015832"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018JB015832"},{"@id":"http://api.wiley.com/onlinelibrary/chorus/v1/articles/10.1029%2F2018JB015832"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB015832"}],"createdAt":"2018-09-19","modifiedAt":"2024-07-10","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256879576576","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"16H06476"},{"@type":"JGN","@value":"JP16H06476"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-16H06476/"}],"notation":[{"@language":"ja","@value":"スロー地震の地質学的描像と摩擦・水理特性の解明"},{"@language":"en","@value":"Study on geological perspectives, frictional and hydrological properties of slow earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257259871104","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26257206"},{"@type":"JGN","@value":"JP26257206"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26257206/"}],"notation":[{"@language":"ja","@value":"沈み込み帯浅部のスロースリップはトラフ軸まで到達するか？"},{"@language":"en","@value":"Slow slip to the trench  ?"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050022708919908096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Synthesizing sea surface height change including seismic waves and tsunami using a dynamic rupture scenario of anticipated Nankai trough earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1050869456404213632","@type":"Article","resourceType":"学術雑誌論文(journal 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earthquakes."}]},{"@id":"https://cir.nii.ac.jp/crid/1390305721537046784","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2024年日向灘の地震に伴う津波の波源分布"},{"@language":"en","@value":"Tsunami Source Modeling of the Earthquake beneath Hyuganada Sea on 8 August 2024 Using Ocean-bottom Pressure Gauge Records of N-net and DONET"},{"@value":"2024年日向灘の地震に伴う津波の波源分布 : N-netとDONETの水圧計記録の解析から"},{"@language":"ja-Kana","@value":"2024ネン ヒュウガナダ ノ ジシン ニ トモナウ ツナミ ノ ナミ ゲン ブンプ : N-net ト DONET ノ スイアツケイ キロク ノ カイセキ カラ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520854805118488704","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ocean Tide Models Developed by Assimilating TOPEX/POSEIDON Altimeter Data into Hydrodynamical Model:A Global Model and a Regional Model around Japan"},{"@language":"ja-Kana","@value":"Ocean Tide Models Developed by Assimilating TOPEX POSEIDON Altimeter Data into Hydrodynamical Model A Global Model and a 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