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Comparison between computed balance velocities and GPS measurements in the Lambert Glacier basin, East Antarctica
Testut, L and Hurd, R and Coleman, R and Frédérique, R and Legresy, B (2003) Comparison between computed balance velocities and GPS measurements in the Lambert Glacier basin, East Antarctica. Annals of Glaciology, 37 (1). pp. 337-343. ISSN 0260-3055
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Comparisons between computed balance velocities, obtained from two different computing schemes, and global positioning system (GPS)-derived velocities were made in the Lambert Glacier basin region, East Antarctica. The two computing schemes used for the balance-velocity computations (a flowline (FL) scheme (Rémy and Minster, 1993) and a finite-difference (BW) scheme (Budd and Warner, 1996; Fricker and others, 2000)) were first evaluated and compared. One of the key issues studied was the spatial resolution of the digital elevation model (DEM), representing the surface topography of the ice sheet, and the sensitivity of the balance velocities to the length of smoothing applied to the DEM. Comparison with the GPS velocities validated the two schemes to within 5-25% but showed the high sensitivity of the flowline method to the length scale of the smoothing. The finite-difference scheme was found to be robust to the chosen smoothing scale, but the balance-velocity values increased when a finer-resolution DEM was used. Both FL and BW computing schemes tended to overestimate the balance velocities in comparison with the GPS values; some of this discrepancy can be attributed to ice-sheet sliding.
|Journal or Publication Title:||Annals of Glaciology|
|Page Range:||pp. 337-343|
|Identification Number - DOI:||10.3189/172756403781815672|
© 2003 International Glaciological Society
|Date Deposited:||23 Feb 2009 03:16|
|Last Modified:||18 Nov 2014 03:55|
|Item Statistics:||View statistics for this item|
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