{ "@context": "http://schema.org/", "@type": "Dataset", "@id": "https://antcat.antarcticanz.govt.nz/geonetwork/srv/api/records/d5409f49-303f-4b69-b679-9455f3ed07a9", "includedInDataCatalog":[{"@type":"DataCatalog","url":"https://antcat.antarcticanz.govt.nz/geonetwork/srv/search#","name":""}], "inLanguage":"eng", "name": "GNSS Data collected at Priestley Glacier November 2018", "alternateName": [ ], "dateCreated": [ "2021-09-22T00:00:00"], "dateModified": [ ], "datePublished": [ "2021-09-22T00:00:00"], "thumbnailUrl": [ "https://antcat.antarcticanz.govt.nz:/geonetwork/srv/api/records/d5409f49-303f-4b69-b679-9455f3ed07a9/attachments/d5409f49-303f-4b69-b679-9455f3ed07a9.png"], "description": "This is GNSS data of four stations covering the grounding zone of Priestley Glacier Antarctica.\n\nTidal modulation of ice streams and their adjacent ice shelves is a real-world experiment to understand ice-dynamic processes. We observe the dynamics of Priestley Glacier, Antarctica, using Terrestrial Radar Interferometry (TRI) and GNSS. Ocean tides are predominantly diurnal but horizontal GNSS displacements oscillate also semi-diurnally. The oscillations are strongest in the ice shelf and tidal signatures decay near-linearly in the TRI data over >10 km upstream of the grounding line. Tidal flexing is observed >6 km upstream of the grounding line including cm-scale uplift. Tidal grounding line migration is small and <40 % of the ice thickness. The frequency doubling of horizontal displacements relative to the ocean tides is consistent with variable ice-shelf buttressing demonstrated with a visco-elastic Maxwell model. Taken together, this supports previously hypothesized flexural ice softening in the grounding-zone through tides and offers new observational constraints for the role of ice rheology in ice-shelf buttressing.\n\nRelated Publication:\nDrews, R., Wild, C. T., Marsh, O. J., Rack, W., Ehlers, T. A., Neckel, N., & Helm, V. (2021). Grounding-zone flow variability of Priestley Glacier, Antarctica, in a diurnal tidal regime. Geophysical Research Letters, 48, e2021GL093853. https:\/\/doi.org\/10.1029\/2021GL093853\n\nGET DATA:\nhttps:\/\/doi.pangaea.de\/10.1594\/PANGAEA.936090", "identifier": "https://doi.org/10.1594/PANGAEA.936090", "keywords":[ "PRIESTLEY GLACIER","INSTALLATION","K050A","GLACIERS","TIDES","OCEANS","GLACIER MOTION\/ICE SHEET MOTION","Global Positioning System (GPS)","GPS","GNSS","ANTARCTICA" ] ,"creator": [ { "@type":"Person" ,"name": "Drews, Reinhard." ,"email": ["reinhard.drews@uni-tuebingen.de"] ,"contactPoint": { "@type" : "PostalAddress" } } ] ,"publisher": [ { "@type":"Organization" ,"name": "PANGAEA" ,"email": ["info@pangaea.de"] ,"contactPoint": { "@type" : "PostalAddress" } } ] ,"distribution": [ { "@type":"DataDownload", "contentUrl": "https:\/\/doi.org\/10.1594\/PANGAEA.936090", "encodingFormat": "WWW:LINK-1.0-http--link", "name": "Distribution Metadata" }] ,"encodingFormat": [ ] ,"spatialCoverage": [ {"@type":"Place", "description": [ ], "geo": [ {"@type":"GeoShape", "box": "-74.526 163.4182 -74.3934 163.458" } ] }] ,"temporalCoverage": [ "2018-11-01T00:00:00/2018-12-29T12:00:00" ] ,"license": [ { "@type": "CreativeWork", "name": "This data set conforms to the CC BY Attribution License (https:\/\/creativecommons.org\/licenses\/by\/4.0\/)" } ] , "citation": "Drews, Reinhard., Wild, Christian T., Marsh, Oliver., Rack, Wolfgang., Ehlers, Todd A., Neckel, Niklas., Helm, Veit., ( 2021 ) GNSS Data collected at Priestley Glacier November 2018. PANGAEA. https://doi.org/10.1594/PANGAEA.936090, Accessed: 2026-07-07+12:00" }