{"@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/1363670320015351040.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/96jb03458"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB03458"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB03458"}},{"identifier":{"@type":"NAID","@value":"30013335675"}}],"dc:title":[{"@value":"NLOADF: A program for computing ocean‐tide loading"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The loading of the Earth by the ocean tides produces several kinds of signals which can be measured by geodetic technique. In order to compute these most accurately, a combination of global and local models of the ocean tides may be needed. The program NLOADF convolves the Green functions for loading with ocean tide models using a station‐centered grid with fixed dimensions, making it easy to combine different ocean models without overlap in the convolution. The program computes all the quantities of interest (gravity, displacement, tilt, and strain) and includes the case where measurements are made beneath the surface of the ocean.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320015351040","@type":"Researcher","foaf:name":[{"@value":"Duncan Carr Agnew"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1997-03-10","prism:volume":"102","prism:number":"B3","prism:startingPage":"5109","prism:endingPage":"5110"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F96JB03458"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/96JB03458"}],"createdAt":"2004-02-03","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360848658212751104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Correlation between the phase of the moon and the occurrences of microearthquakes in the Tamba region through point‐process modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1520572358210017536","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Map Projections to Represent Possible Effects of Surface Loading"},{"@language":"ja-Kana","@value":"Map Projections to Represent Possible Effects of Surface Loading"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668923994779776","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"断層運動で生じた静的応力の増大が引き起こした地球潮汐による地震誘発現象"},{"@language":"en","@value":"Tidal triggering of earthquakes enhanced by static stress changes"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/96jb03458"},{"@type":"CIA","@value":"30013335675"},{"@type":"CROSSREF","@value":"10.1029/2005gl025510_references_DOI_ZuC1HAk4Qx2BhUKL7Zg7JZcfkrm"}]}