Ice-sheet elevations from across-track processing of airborne interferometric radar altimetry


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Veit.Helm [ at ] awi.de

Abstract

Interferometric Radar Altimeters (IRA's) use dual receive antennas to overcome one of the spatial limitations of pulse-limited altimeters. In a conventional IRA measurement, the range and across-track direction of a scatterer are determined using the phase difference between the antennas. We demonstrate a method of determining multiple elevation points across a swath orthogonal to the instrument ground track in regions of steep terrain, such as ice-sheet margins. We use data from an airborne IRA (a prototype of the CryoSat-2 instrument), and compare the results to simultaneous Airborne Laser Scanner (ALS) observations. This application results in a 75-fold increase in measurement density compared to conventional radar altimetry. Along a ∼2.5 km ground track, the RMS departure between the IRA- and ALS-derived measurements was 1.67 m. Based on our result, although our approach is limited to areas of relatively steep slope, a 25- to 75-fold increase in elevation measurements could be achieved in coastal regions of Antarctica and Greenland with similar processing of CryoSat-2 data.



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Article
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ISI/Scopus peer-reviewed
Publication Status
Published
Eprint ID
21155
DOI 10.1029/2009GL040416

Cite as
Hawley, R. L. , Sheperd, A. , Cullen, R. , Helm, V. and Wingham, D. J. (2009): Ice-sheet elevations from across-track processing of airborne interferometric radar altimetry , Geophysical Research Letters., 36 (L22501) . doi: 10.1029/2009GL040416


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