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

被引:11
作者
Cartwright, Jessica [1 ,2 ,3 ]
Banks, Christopher J. [4 ]
Srokosz, Meric [1 ]
机构
[1] Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England
[2] Natl Oceanog Ctr, Ocean & Earth Sci, Southampton, Hants, England
[3] Univ Southampton, Southampton SO14 3ZH, Hants, England
[4] Natl Oceanog Ctr, Liverpool L3 5DA, Merseyside, England
基金
英国自然环境研究理事会;
关键词
GPS SIGNALS; DOME C; SCATTERING; SNOW; REFLECTOMETRY; OCEAN; INTERFEROMETRY; PRECISION; RADAR;
D O I
10.5194/tc-14-1909-2020
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
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 degrees 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.
引用
收藏
页码:1909 / 1917
页数:9
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