{"data":{"id":"10.4121/uuid:da761d33-2e37-41e9-af6b-cd4b8d588e55","type":"dois","attributes":{"doi":"10.4121/uuid:da761d33-2e37-41e9-af6b-cd4b8d588e55","prefix":"10.4121","suffix":"uuid:da761d33-2e37-41e9-af6b-cd4b8d588e55","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Stef Lhermitte","nameType":"Personal","familyName":"Stef Lhermitte","nameIdentifiers":[{"nameIdentifier":"0000-0002-1622-0177","nameIdentifierScheme":"https://orcid.org/"}],"affiliation":[]},{"name":"Wouters, Bert","nameType":"Personal","givenName":"Bert","familyName":"Wouters","nameIdentifiers":[{"nameIdentifier":"0000-0002-1086-2435","nameIdentifierScheme":"https://orcid.org/"}],"affiliation":[]}],"titles":[{"title":"Data from Cryosat-2 satellite showing elevation change over Pine Island Glacier and Thwaites Glacier"}],"publisher":"4TU.ResearchData","container":{},"publicationYear":2020,"subjects":[{"subject":"Physical Geography and Environmental Geoscience","subjectScheme":"Australian and New Zealand Standard Research Classification (ANZSRC), 2008","classificationCode":"0406"},{"subject":"FOS: Earth and related environmental sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Other Earth Sciences","subjectScheme":"Australian and New Zealand Standard Research Classification (ANZSRC), 2008","classificationCode":"0499"},{"subject":"Antarctica"},{"subject":"Cryosat-2"},{"subject":"Geomatic Engineering"},{"subject":"FOS: Environmental engineering","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Time: 2010-2017"}],"contributors":[{"name":"TU Delft, Faculty Of Civil Engineering And Geosciences, Department Of Geoscience \u0026 Remote Sensing","nameType":"Organizational","affiliation":[],"contributorType":"Other","nameIdentifiers":[]}],"dates":[{"date":"2020-08-21","dateType":"Issued"}],"language":"en","types":{"ris":"DATA","bibtex":"misc","citeproc":"dataset","schemaOrg":"Dataset","resourceType":"Dataset","resourceTypeGeneral":"Dataset"},"relatedIdentifiers":[],"relatedItems":[],"sizes":[],"formats":["media types: application/zip, image/tiff"],"version":"1","rightsList":[{"rights":"Creative Commons Attribution Share Alike 4.0 International","rightsUri":"https://creativecommons.org/licenses/by-sa/4.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-sa-4.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"description":"Rates of elevation change for 2010-2017 derived from interferometric measurements from Cryosat-2. Elevation change was derived from interferometric measurements from Cryosat-2. ESA L1b waveforms retrieved by the satellite in its SARIn (synthetic aperture radar interferometry) mode were processed following the swath processing approach of Gray et al(2013). The resulting dense set of time-dependent elevation measurements was used to derive elevation changes in a Eulerian framework at a 500 m resolution following the method presented in Wouters et al. (2015).","descriptionType":"Abstract"}],"geoLocations":[{"geoLocationPlace":"Amundsen Sea Embayment"}],"fundingReferences":[{"awardTitle":"Nederlandse Organisatie voor Wetenschappelijk Onderzoek, 016.Vidi.171.065","funderName":"unknown"},{"awardTitle":"Nederlandse Organisatie voor Wetenschappelijk Onderzoek, 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