{ "@context": "http://schema.org/", "@type": "Dataset", "@id": "https://antcat.antarcticanz.govt.nz/geonetwork/srv/api/records/0e73c346-8421-4fe0-ac2d-7af099fb9990", "includedInDataCatalog":[{"@type":"DataCatalog","url":"https://antcat.antarcticanz.govt.nz/geonetwork/srv/search#","name":""}], "inLanguage":"eng", "name": "Global Glacioisostatic Adjustment (GIA) and Ice Sheet Model Output, West Antarctic Ice Sheet Holocene Retreat\/Readvance", "alternateName": [ ], "dateCreated": [ "2024-04-23T00:00:00"], "dateModified": [ ], "datePublished": [ "2024-04-23T00:00:00"], "thumbnailUrl": [ "https://antcat.antarcticanz.govt.nz/geonetwork/srv/api/records/0e73c346-8421-4fe0-ac2d-7af099fb9990/attachments/0e73c346-8421-4fe0-ac2d-7af099fb9990.png"], "description": "The ice sheet model outputs include Antarctic bed topography, ice thickness, and ice sheet mask (i.e. bedrock, grounded ice, floating ice, open ocean). Outputs are at 500 year intervals from 9.5 to 0 ka, but 100 year temporal resolution is available on request.\n\nFile naming convention is as follows: hotf = Holocene ocean thermal forcing anomaly, mv = mantle viscosity, lfr = lithosphere flexural rigidity.\n\nThe GIA model outputs include global bed topography at intervals of 100 years.\n\nRelated Publication: Lowry, D.P., Han, H.K., Golledge, N.R. et al. Ocean cavity regime shift reversed West Antarctic grounding line retreat in the late Holocene. Nat Commun 15, 3176 (2024). https:\/\/doi.org\/10.1038\/s41467-024-47369-3\n\nGET DATA: https:\/\/osf.io\/xqs8w\/", "identifier": "https://doi.org/10.1038/s41467-024-47369-3", "keywords":[ "","Earth Science | Paleoclimate","Earth Science | Climate Indicators | Paleoclimate Indicators | Paleoclimate Reconstructions","Other | Models","In Situ\/Laboratory Instruments | Data Analysis | Environmental Modeling","Continent | Antarctica","ASP" ] ,"creator": [ { "@type":"Person" ,"name": "Lowry, D.P." ,"email": [""] ,"contactPoint": { "@type" : "PostalAddress" } } ] ,"publisher": [ { "@type":"Organization" ,"name": "Nature Communications" ,"email": [""] ,"contactPoint": { "@type" : "PostalAddress" } } ] ,"distribution": [ { "@type":"DataDownload", "contentUrl": "https:\/\/antcat.antarcticanz.govt.nz\/geonetwork\/srv\/api\/records\/0e73c346-8421-4fe0-ac2d-7af099fb9990", "encodingFormat": "WWW:LINK-1.0-http--link", "name": "Distribution Metadata" }] ,"encodingFormat": [ ] ,"spatialCoverage": [ {"@type":"Place", "description": [ ], "geo": [ {"@type":"GeoShape", "box": "-88.00 -180.00 -68.00 -160.00" }, {"@type":"GeoShape", "box": "-88.00 160.00 -68.00 180.00" } ] }] ,"temporalCoverage": [ "2024-04-23/2024-04-23" ] ,"license": [ { "@type": "CreativeWork", "name": "This data set conforms to the CC BY Attribution License (https:\/\/creativecommons.org\/licenses\/by\/4.0\/)" } ] , "citation": "Lowry, D.P., Han, H.K., Golledge, N.R., Gomez, N., Johnson, K.M., McKay, R.M., ( 2024 ) Global Glacioisostatic Adjustment (GIA) and Ice Sheet Model Output, West Antarctic Ice Sheet Holocene Retreat/Readvance. Nature Communications. https://doi.org/10.1038/s41467-024-47369-3, Accessed: 2026-07-07+12:00" }