The Reference Elevation Model of Antarctica
The Reference Elevation Model of Antarctica (REMA) is the first continental-scale digital elevation model (DEM) at a resolution of less than 10 m. REMA is created from stereophotogrammetry with submeter resolution optical, commercial satellite imagery. The higher spatial and radiometric resolutions...
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Online Access: | https://doi.org/10.5194/tc-13-665-2019 https://tc.copernicus.org/articles/13/665/2019/ |
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ftcopernicus:oai:publications.copernicus.org:tc72656 2023-05-15T13:55:28+02:00 The Reference Elevation Model of Antarctica Howat, Ian M. Porter, Claire Smith, Benjamin E. Noh, Myoung-Jong Morin, Paul 2019-02-26 application/pdf https://doi.org/10.5194/tc-13-665-2019 https://tc.copernicus.org/articles/13/665/2019/ eng eng doi:10.5194/tc-13-665-2019 https://tc.copernicus.org/articles/13/665/2019/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-13-665-2019 2020-07-20T16:22:55Z The Reference Elevation Model of Antarctica (REMA) is the first continental-scale digital elevation model (DEM) at a resolution of less than 10 m. REMA is created from stereophotogrammetry with submeter resolution optical, commercial satellite imagery. The higher spatial and radiometric resolutions of this imagery enable high-quality surface extraction over the low-contrast ice sheet surface. The DEMs are registered to satellite radar and laser altimetry and are mosaicked to provide a continuous surface covering nearly 95 % the entire continent. The mosaic includes an error estimate and a time stamp, enabling change measurement. Typical elevation errors are less than 1 m, as validated by the comparison to airborne laser altimetry. REMA provides a powerful new resource for Antarctic science and provides a proof of concept for generating accurate high-resolution repeat topography at continental scales. Text Antarc* Antarctic Antarctica Ice Sheet Copernicus Publications: E-Journals Antarctic The Cryosphere 13 2 665 674 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The Reference Elevation Model of Antarctica (REMA) is the first continental-scale digital elevation model (DEM) at a resolution of less than 10 m. REMA is created from stereophotogrammetry with submeter resolution optical, commercial satellite imagery. The higher spatial and radiometric resolutions of this imagery enable high-quality surface extraction over the low-contrast ice sheet surface. The DEMs are registered to satellite radar and laser altimetry and are mosaicked to provide a continuous surface covering nearly 95 % the entire continent. The mosaic includes an error estimate and a time stamp, enabling change measurement. Typical elevation errors are less than 1 m, as validated by the comparison to airborne laser altimetry. REMA provides a powerful new resource for Antarctic science and provides a proof of concept for generating accurate high-resolution repeat topography at continental scales. |
format |
Text |
author |
Howat, Ian M. Porter, Claire Smith, Benjamin E. Noh, Myoung-Jong Morin, Paul |
spellingShingle |
Howat, Ian M. Porter, Claire Smith, Benjamin E. Noh, Myoung-Jong Morin, Paul The Reference Elevation Model of Antarctica |
author_facet |
Howat, Ian M. Porter, Claire Smith, Benjamin E. Noh, Myoung-Jong Morin, Paul |
author_sort |
Howat, Ian M. |
title |
The Reference Elevation Model of Antarctica |
title_short |
The Reference Elevation Model of Antarctica |
title_full |
The Reference Elevation Model of Antarctica |
title_fullStr |
The Reference Elevation Model of Antarctica |
title_full_unstemmed |
The Reference Elevation Model of Antarctica |
title_sort |
reference elevation model of antarctica |
publishDate |
2019 |
url |
https://doi.org/10.5194/tc-13-665-2019 https://tc.copernicus.org/articles/13/665/2019/ |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-13-665-2019 https://tc.copernicus.org/articles/13/665/2019/ |
op_doi |
https://doi.org/10.5194/tc-13-665-2019 |
container_title |
The Cryosphere |
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13 |
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2 |
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665 |
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674 |
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1766262117569134592 |