{"@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/1360004233291826432.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2018gl080830"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018GL080830"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080830"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018GL080830"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1029/2018GL080830"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080830"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Seafloor Crustal Deformation on Ocean Bottom Pressure Records With Nontidal Variability Corrections: Application to Hikurangi Margin, New Zealand"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Ocean bottom pressure (OBP) observations are a powerful tool for determining vertical crustal displacements, especially due to earthquakes and slow earthquakes, with centimeter‐level resolution. In these studies, removal of oceanographic noise (tens of centimeters) is required to identify centimeter‐level crustal deformation. We undertake barotropic modeling to remove oceanographic signals from data from an OBP array deployed offshore New Zealand in 2014/2015. We show that removing the nontidal component calculated from a barotropic ocean model reduces the variance in the data by about 66% and provides a feasible means to resolve pressure changes due to crustal deformation during the slow slip events. We also discuss the vertical displacements from slow slip events that occurred in late September to mid‐October 2014, and we outline our procedure for processing OBP data.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276176739072","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60828284"},{"@type":"NRID","@value":"1000060828284"},{"@type":"NRID","@value":"9000410904571"},{"@type":"NRID","@value":"9000375922136"},{"@type":"NRID","@value":"9000406397651"},{"@type":"NRID","@value":"9000415314237"},{"@type":"NRID","@value":"9000405892840"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/muramura_143"}],"foaf:name":[{"@value":"Tomoya Muramoto"}],"jpcoar:affiliationName":[{"@value":"Research Center for Earthquake Prediction, Disaster Prevention Research Institute Kyoto University  Uji Japan"},{"@value":"Now at National Metrology Institute of Japan National Institute of Advanced Industrial Science and Technology  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":"Research Center for Earthquake Prediction, Disaster Prevention Research Institute Kyoto University  Uji Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233291826304","@type":"Researcher","foaf:name":[{"@value":"Daisuke Inazu"}],"jpcoar:affiliationName":[{"@value":"Department of Marine Resource and Energy Tokyo University of Marine Science and Technology  Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233291826306","@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/1380004233291826310","@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/1380004233291826305","@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/1380004233291826432","@type":"Researcher","foaf:name":[{"@value":"Spahr C. Webb"}],"jpcoar:affiliationName":[{"@value":"Lamont‐Doherty Earth Observatory Columbia University  Palisades NY USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233291826307","@type":"Researcher","foaf:name":[{"@value":"Stuart Henrys"}],"jpcoar:affiliationName":[{"@value":"GNS Science  Lower Hutt New Zealand"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2019-01-13","prism:volume":"46","prism:number":"1","prism:startingPage":"303","prism:endingPage":"310"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#am","http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018GL080830"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080830"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018GL080830"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1029/2018GL080830"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080830"}],"createdAt":"2018-12-28","modifiedAt":"2023-09-09","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/1050292561229551360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Water Depth Dependence of Long‐Range Correlation in Nontidal Variations in Seafloor Pressure"},{"@value":"Water depth dependence of long-range correlation in nontidal variations in seafloor 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