Slope, aspect, Antarctic ice sheet, ICESat, repeat orbit
Digital Object Identifier (DOI)
Accurate information of ice sheet surface slope is essential for estimating elevation change by satellite altimetry measurement. A study is carried out to recover surface slope of Antarctic ice sheet from Ice, Cloud and land Elevation Satellite (ICESat) elevation measurements based on repeat orbits. ICESat provides repeat ground tracks within 200 meters in cross-track direction and 170 meters in along-track direction for most areas of Antarctic ice sheet. Both cross-track and along-track surface slopes could be obtained by adjacent repeat ground tracks. Combining those measurements yields a surface slope model with resolution of approximately 200 meters. An algorithm considering elevation change is developed to estimate the surface slope of Antarctic ice sheet. Three Antarctic Digital Elevation Models (DEMs) were used to calculate surface slopes. The surface slopes from DEMs are compared with estimates by using in situ GPS data in Dome A, the summit of Antarctic ice sheet. Our results reveal an average surface slope difference of 0.02 degree in Dome A. High resolution remote sensing images are also used in comparing the results derived from other DEMs and this paper. The comparison implies that our results have a slightly better coherence with GPS observation than results from DEMs, but our results provide more details and perform higher accuracy in coastal areas because of the higher resolution for ICESat measurements. Ice divides are estimated based on the aspect, and are weakly consistent with ice divides from other method in coastal regions.
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Citation / Publisher Attribution
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, v. XLII-2-W7, p. 1579-1583
Scholar Commons Citation
Yuan, L.; Li, F.; Zhang, S.; Xie, Surui; Xiao, F.; Zhu, T.; and Zhang, Y., "Antarctic Ice Sheet Slope and Aspect Based on ICESAT's Repeat Orbit Measurement" (2017). School of Geosciences Student Publications. 27.