{"@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/1362262943399426816.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2017gl076623"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL076623"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL076623"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL076623"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL076623"}}],"dc:title":[{"@value":"Combining InSAR and GPS to Determine Transient Movement and Thickness of a Seasonally Active Low‐Gradient Translational Landslide"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The combined application of continuous Global Positioning System data (high temporal resolution) with spaceborne interferometric synthetic aperture radar data (high spatial resolution) can reveal much more about the complexity of large landslide movement than is possible with geodetic measurements tied to only a few specific measurement sites. This approach is applied to an ~4 km<jats:sup>2</jats:sup> reactivated translational landslide in the Columbia River Gorge (Washington State), which moves mainly during the winter rainy season. Results reveal the complex three‐dimensional shape of the landslide mass, how onset of sliding relates to cumulative rainfall, how surface velocity during sliding varies with location on the topographically complex landslide surface, and how the ground surface subsides slightly in weeks prior to downslope sliding.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943399426817","@type":"Researcher","foaf:name":[{"@value":"Xie Hu"}],"jpcoar:affiliationName":[{"@value":"Huffington Department of Earth Sciences Southern Methodist University  Dallas TX USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943399426816","@type":"Researcher","foaf:name":[{"@value":"Zhong Lu"}],"jpcoar:affiliationName":[{"@value":"Huffington Department of Earth Sciences Southern Methodist University  Dallas TX USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943399426818","@type":"Researcher","foaf:name":[{"@value":"Thomas C. Pierson"}],"jpcoar:affiliationName":[{"@value":"U.S. Geological Survey  Vancouver WA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943399426819","@type":"Researcher","foaf:name":[{"@value":"Rebecca Kramer"}],"jpcoar:affiliationName":[{"@value":"U.S. Geological Survey  Vancouver WA USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262943399426688","@type":"Researcher","foaf:name":[{"@value":"David L. George"}],"jpcoar:affiliationName":[{"@value":"U.S. Geological Survey  Vancouver WA 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":"2018-02-15","prism:volume":"45","prism:number":"3","prism:startingPage":"1453","prism:endingPage":"1462"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2017GL076623"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL076623"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2017GL076623"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL076623"}],"createdAt":"2018-02-02","modifiedAt":"2025-05-16","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360302865745869312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of Landslides Due to the Combined Disaster of Earthquake and Heavy Rainfall Using Multi-Temporal Lidar Data"}]},{"@id":"https://cir.nii.ac.jp/crid/1363101969073633536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of Earthquake-Induced Landslides during the 2018 Kumamoto Earthquake Using Multitemporal Airborne Lidar Data"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367075039360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal behavior of a large-scale landslide at Mt. 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