{"@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/1360011144655214848.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2013gl058295"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058295"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2013GL058295"}}],"dc:title":[{"@value":"Isotropic thaw subsidence in undisturbed permafrost landscapes"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Observations in undisturbed terrain within some regions of the Arctic reveal limited correlation between increasing air temperature and the thickness of the seasonally thawed layer above ice‐rich permafrost. Here we describe landscape‐scale, thaw‐induced subsidence lacking the topographic contrasts associated with thermokarst terrain. A high‐resolution, 11 year record of temperature and vertical movement at the ground surface from contrasting physiographic regions of northern Alaska, obtained with differential global positioning systems technology, indicates that thaw of an ice‐rich layer at the top of permafrost has produced decimeter‐scale subsidence extending over the entire landscapes. Without specialized observation techniques the subsidence is not apparent to observers at the surface. This “isotropic thaw subsidence” explains the apparent stability of active layer thickness records from some landscapes of northern Alaska, despite warming near‐surface air temperatures. Integrated over extensive regions, it may be responsible for thawing large volumes of carbon‐rich substrate and could have negative impacts on infrastructure.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011144655214848","@type":"Researcher","foaf:name":[{"@value":"Nikolay I. Shiklomanov"}],"jpcoar:affiliationName":[{"@value":"Department of Geography The George Washington University  Washington D.C. USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144655214849","@type":"Researcher","foaf:name":[{"@value":"Dmitry A. Streletskiy"}],"jpcoar:affiliationName":[{"@value":"Department of Geography The George Washington University  Washington D.C. USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144655214976","@type":"Researcher","foaf:name":[{"@value":"Jonathon D. Little"}],"jpcoar:affiliationName":[{"@value":"Monroe Community College  Rochester New York USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144655214850","@type":"Researcher","foaf:name":[{"@value":"Frederick E. Nelson"}],"jpcoar:affiliationName":[{"@value":"Department of Geography University of Delaware  Newark Delaware 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":"2013-12-18","prism:volume":"40","prism:number":"24","prism:startingPage":"6356","prism:endingPage":"6361"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2013GL058295"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2013GL058295"}],"createdAt":"2013-12-11","modifiedAt":"2023-10-03","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360017282426702592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Transient Freeze‐Thaw Deformation Responses to the 2018 and 2019 Fires Near Batagaika Megaslump, Northeast Siberia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429441049856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thawing permafrost is subsiding in the Northern Hemisphere—review and perspectives"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285714493682688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"InSAR Detection and Field Evidence for Thermokarst after a Tundra Wildfire, Using ALOS-PALSAR"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617435182720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Post‐Wildfire Surface Deformation Near Batagay, Eastern Siberia, Detected by L‐Band and C‐Band InSAR"}]},{"@id":"https://cir.nii.ac.jp/crid/1360564064127213184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pan-Arctic ice-wedge degradation in warming permafrost and its influence on tundra hydrology"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266981883776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface displacement revealed by L-band InSAR analysis in the Mayya area, Central Yakutia, underlain by continuous permafrost"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2013gl058295"},{"@type":"CROSSREF","@value":"10.1029/2022jf006817_references_DOI_ST2IlCCicddCAJXd1E8ZGQyqrsU"},{"@type":"CROSSREF","@value":"10.1088/1748-9326/ada2ff_references_DOI_ST2IlCCicddCAJXd1E8ZGQyqrsU"},{"@type":"CROSSREF","@value":"10.3390/rs8030218_references_DOI_ST2IlCCicddCAJXd1E8ZGQyqrsU"},{"@type":"CROSSREF","@value":"10.1029/2019jf005473_references_DOI_ST2IlCCicddCAJXd1E8ZGQyqrsU"},{"@type":"CROSSREF","@value":"10.1038/ngeo2674_references_DOI_ST2IlCCicddCAJXd1E8ZGQyqrsU"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01266-3_references_DOI_ST2IlCCicddCAJXd1E8ZGQyqrsU"}]}