{"@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/1363388843896005376.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2003gl019150"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2003GL019150"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003GL019150"}}],"dc:title":[{"@value":"Detection of arbitrarily large dynamic ground motions with a dense high‐rate GPS network"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We describe the detection of teleseismic surface waves from the 3 November 2002 Mw 7.9 Denali fault earthquake in Alaska with a dense network of 1 Hz GPS stations in southern California, about 3900 km from the event. Relative horizontal displacements with amplitudes in excess of 15 mm and duration of 700 seconds agree with integrated velocities recorded by nearby broadband seismometers with an rms difference of 2–3 mm. The displacements are derived from independent 1 Hz instantaneous positions demonstrating that a GPS network can provide direct measurements of arbitrarily large dynamic and static ground horizontal displacements at periods longer than 1 s and amplitudes above 2 mm, with an inherent precision (signal to noise) that improves indefinitely with amplitude without clipping and in real time. High‐rate, real‐time GPS networks can enhance earthquake detection and seismic risk mitigation and support other applications such as intelligent transportation and civil infrastructure monitoring.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388843896005376","@type":"Researcher","foaf:name":[{"@value":"Yehuda Bock"}],"jpcoar:affiliationName":[{"@value":"Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics Scripps Institution of Oceanography  La Jolla California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843896005377","@type":"Researcher","foaf:name":[{"@value":"Linette Prawirodirdjo"}],"jpcoar:affiliationName":[{"@value":"Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics Scripps Institution of Oceanography  La Jolla California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843896005378","@type":"Researcher","foaf:name":[{"@value":"Timothy I. Melbourne"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences Central Washington University  Ellensburg Washington USA"}]}],"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":"2004-03","prism:volume":"31","prism:number":"6","prism:startingPage":"L06604"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2003GL019150"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003GL019150"}],"createdAt":"2004-03-17","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285708831334528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New Geometric Restriction for the Displacement–Constraint Points in Discontinuous Deformation Analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641639189888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quasi real‐time fault model estimation for near‐field tsunami forecasting based on RTK‐GPS analysis: Application to the 2011 Tohoku‐Oki earthquake (<i>M</i><sub>w</sub> 9.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489147648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A decade of GEONET: 1994-2003"},{"@value":"A decade of GEONET: 1994-2003--The continuous GPS observation in Japan and its impact on earthquake studies"},{"@language":"ja-Kana","@value":"decade of GEONET 1994 2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003 —The continuous GPS observation in Japan and its impact on earthquake studies—"},{"@value":"1994–2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observations in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observation in Japan and its impact on earthquake studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763128053120","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Review on Near-Field Tsunami Forecasting from Offshore Tsunami Data and Onshore GNSS Data for Tsunami Early Warning"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588891959347456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Source process with heterogeneous rupture velocity for the 2011 Tohoku-Oki earthquake based on 1-Hz GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892106671616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the performance of position-domain sidereal filter for 30-s kinematic GPS to mitigate multipath errors"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317068482944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic characteristics of very-high-rate GPS observations for seismology"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2003gl019150"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0572-4_references_DOI_6CVSNXu2ZwCHSBi5kvc58u0Lyth"},{"@type":"CROSSREF","@value":"10.1061/(asce)gm.1943-5622.0000648_references_DOI_6CVSNXu2ZwCHSBi5kvc58u0Lyth"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0339_references_DOI_6CVSNXu2ZwCHSBi5kvc58u0Lyth"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.11.005_references_DOI_6CVSNXu2ZwCHSBi5kvc58u0Lyth"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01584-8_references_DOI_6CVSNXu2ZwCHSBi5kvc58u0Lyth"},{"@type":"CROSSREF","@value":"10.1029/2011jb008750_references_DOI_6CVSNXu2ZwCHSBi5kvc58u0Lyth"},{"@type":"CROSSREF","@value":"10.1186/bf03353077_references_DOI_6CVSNXu2ZwCHSBi5kvc58u0Lyth"}]}