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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Bibliographic Details
Published in:The Cryosphere
Main Authors: I. M. Howat, C. Porter, B. E. Smith, M.-J. Noh, P. Morin
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Environmental sciences
GE1-350
Geology
QE1-996.5
Antarctic
Antarc*
Antarctica
Ice Sheet
The Cryosphere
Online Access:https://doi.org/10.5194/tc-13-665-2019
https://doaj.org/article/3bbfa67d7f02425f883fb3337f29740d
Description
Summary: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.

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