{"@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/1362262945793848448.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2019ea000662"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2019EA000662"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019EA000662"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019EA000662"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019EA000662"}}],"dc:title":[{"@value":"Landslide Scaling: A Review"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Key Points</jats:title><jats:p>\n<jats:list list-type=\"bullet\">\n<jats:list-item><jats:p>Size‐frequency distributions of landslides are well described by a power function for events with areas larger than 10,000 m<jats:sup>2</jats:sup></jats:p></jats:list-item>\n<jats:list-item><jats:p>Landslide scaling has been modeled with self‐organized criticality, non‐parameterized cellular automata models, and mechanical models</jats:p></jats:list-item>\n</jats:list></jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380572092771093632","@type":"Researcher","foaf:name":[{"@value":"S. F. Tebbens"}],"jpcoar:affiliationName":[{"@value":"Department of Physics Wright State University  Dayton OH USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"23335084"},{"@type":"EISSN","@value":"23335084"}],"prism:publicationName":[{"@value":"Earth and Space Science"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2020-01","prism:volume":"7","prism:number":"1","prism:startingPage":"e2019EA000662"},"reviewed":"false","dc:rights":["http://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2019EA000662"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019EA000662"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2019EA000662"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019EA000662"}],"createdAt":"2019-11-08","modifiedAt":"2023-09-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/2050307417125248384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Classification of topography for ground vulnerability assessment of alluvial plains and mountains of Japan using 30 m DEM"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2019ea000662"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00398-0_references_DOI_FoGjRQppLtwzNI2jAa7DoGmI96a"}]}