Improved GNSS-R bi-static altimetry and independent digital elevation models of Greenland and Antarctica from TechDemoSat-1

• Published in: The Cryosphere
• Main Authors: J. Cartwright, C. J. Banks, M. Srokosz
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2020
• Subjects: Environmental sciences; GE1-350; Geology; QE1-996.5; Antarctic; Cartwright; Greenland; South Pole; The Antarctic; Antarc*; Antarctica; South pole; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-14-1909-2020; https://doaj.org/article/eba9c84f73554e90b57cc4555a565444

Improved digital elevation models (DEMs) of the Antarctic and Greenland ice sheets are presented, which have been derived from Global Navigation Satellite Systems-Reflectometry (GNSS-R). This builds on a previous study (Cartwright et al., 2018) using GNSS-R to derive an Antarctic DEM but uses improved processing and an additional 13 months of measurements, totalling 46 months of data from the UK TechDemoSat-1 satellite. A median bias of under 10 m and root-mean-square errors (RMSEs) of under 53 m for the Antarctic and 166 m for Greenland are obtained, as compared to existing DEMs. The results represent, compared to the earlier study, a halving of the median bias to 9 m , an improvement in coverage of 18 %, and a 4 times higher spatial resolution (now gridded at 25 km ). In addition, these are the first published satellite altimetry measurements of the region surrounding the South Pole. Comparisons south of 88 ∘ S yield RMSEs of less than 33 m when compared to NASA's Operation IceBridge measurements. Differences between DEMs are explored, the limitations of the technique are noted, and the future potential of GNSS-R for glacial ice studies is discussed.