{"@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/1362262946154287360.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1007/s11001-012-9151-7"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s11001-012-9151-7.pdf"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1007/s11001-012-9151-7/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1007/s11001-012-9151-7"}}],"dc:title":[{"@value":"A global barotropic ocean model driven by synoptic atmospheric disturbances for detecting seafloor vertical displacements from in situ ocean bottom pressure measurements"}],"description":[{"notation":[{"@value":"A global barotropic ocean model forced by atmospheric disturbances is developed for the detection of seafloor vertical displacements from in situ ocean bottom pressure (OBP) data. The model accuracy is validated by deep-sea OBP data at more than 100 sites obtained over the global ocean. Parameters and boundary conditions including the horizontal resolution incorporated in the ocean model are tested in order to accurately simulate the nontidal (>2 days) OBP variations. The horizontal resolution is found to the factor that most significantly affects the simulated result. The finer the horizontal resolution applied, the smaller the model variability is. The model accuracy is highest when the horizontal resolution is 1/12°, but deteriorates when the horizontal resolution is finer than 1/12°. This may indicate a failure of the energy dissipation parameterization in the barotropic ocean model. Using the developed 1/12° model, the root-mean-square of the observed nontidal OBP component can be reduced by 18 % as an average of all the OBP data used. It is found that the 1/12° model is useful for the detection of a slow seafloor vertical displacement of centimeters related to the 2011 Tohoku-Oki earthquake from in situ OBP records near the hypocenter of the earthquake."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262946154287360","@type":"Researcher","foaf:name":[{"@value":"Daisuke Inazu"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946154287489","@type":"Researcher","foaf:name":[{"@value":"Ryota Hino"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946154287488","@type":"Researcher","foaf:name":[{"@value":"Hiromi Fujimoto"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00253235"},{"@type":"EISSN","@value":"15730581"}],"prism:publicationName":[{"@value":"Marine Geophysical Research"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2012-05-29","prism:volume":"33","prism:number":"2","prism:startingPage":"127","prism:endingPage":"148"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://link.springer.com/content/pdf/10.1007/s11001-012-9151-7.pdf"},{"@id":"http://link.springer.com/article/10.1007/s11001-012-9151-7/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1007/s11001-012-9151-7"}],"createdAt":"2012-05-28","modifiedAt":"2019-06-01","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 pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216175330176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Episodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230362713856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigation on the Postseismic Deformation Associated with the 2011 Tohoku Earthquake Based on Terrestrial and Seafloor Geodetic Observations: To Evaluate the Further Seismic Hazard Potential on the Plate Interface Beneath the Northeastern Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233291826432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seafloor Crustal Deformation on Ocean Bottom Pressure Records With Nontidal Variability Corrections: Application to Hikurangi Margin, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236864452736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ocean bottom pressure records of the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142696467712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ultrabroadband Seismic and Tsunami Wave Observation of High‐Sampling Ocean‐Bottom Pressure Gauge Covering Periods From Seconds to Hours"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142900996864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of Ocean Fluid Changes on Pressure on the Seafloor: Ocean Assimilation Data Analysis on Warm-Core Rings off the Southeastern Coast of Hokkaido, Japan on an Interannual Timescale"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870443278592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Abrupt water temperature increases near seafloor during the 2011 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643770209920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Editorial: Frontiers in Seafloor Geodesy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294647368684160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Meteotsunami observed by the deep-ocean seafloor pressure gauge network off northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181368426752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global tsunami simulation using a grid rotation transformation in a latitude–longitude coordinate system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092737492864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Improving Detectability of Seafloor Deformation From Bottom Pressure Observations Using Numerical Ocean Models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339757736448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reduction of non-tidal oceanographic fluctuations in ocean-bottom pressure records of DONET using principal component analysis to enhance transient tectonic detectability"}]},{"@id":"https://cir.nii.ac.jp/crid/1360585254927006848","@type":"Article","resourceType":"preprint","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reduction of non-tidal oceanographic fluctuations in ocean bottom pressure records of DONET using principal component analysis to enhance tectonic transient detectability"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417136234368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Assessment of S-net seafoor pressure data quality in view of seafoor geodesy"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1007/s11001-012-9151-7"},{"@type":"OPENAIRE","@value":"doi_dedup___::9727e519c83ee71f805880fe84533771"},{"@type":"CROSSREF","@value":"10.1007/1345_2015_162_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1029/2018gl080830_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1190/segj112013-117_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1029/2020ea001197_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.600930_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1029/2020gl092173_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00556-0_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.744217_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1007/s11069-015-1995-0_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.598270_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1029/2021gl094255_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01862-z_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.21203/rs.3.rs-2604229/v1_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.21203/rs.3.rs-2040866/v1_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2012.08.022_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00526-y_references_DOI_7U0POIvSQzcs9gGA128tz8oktjH"}]}