Journal cover Journal topic
The Cryosphere An interactive open-access journal of the European Geosciences Union
doi:10.5194/tc-2016-277
© Author(s) 2016. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
21 Dec 2016
Review status
This discussion paper is under review for the journal The Cryosphere (TC).
Improved processing and calibration of the interferometric mode of the CryoSat radar altimeter allows height measurements of supraglacial lakes in west Greenland
Laurence Gray1, David Burgess2, Luke Copland1, Thorben Dunse3, Kirsty Langley4, and Geir Moholdt5 1Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, K1N 6N5, Canada
2GSC NRCan, Ottawa, K1A 0E8, Canada
3Department of Geosciences, University of Oslo, 0316 Oslo, Norway
4Asiaq, Greenland Survey, 3900 Nuuk, Greenland
5Norwegian Polar Institute, NO-9296 Tromso, Norway
Abstract. We compare geocoded heights derived from the interferometric mode (SARIn) of CryoSat to surface heights from calibration-validation sites on Devon Ice Cap and West Greenland. Comparisons are included for both the heights derived from the first return (the "point-of-closest-approach" or POCA) as well as heights derived from delayed waveform returns ("swath" processing). While swath processed heights are normally less accurate than edited POCA heights, of order 1–5 m instead of order 1–2 m, the increased coverage possible with swath data complements the POCA data and provides useful information for both system calibration and improving digital elevation models (DEMs). We show that the pre-launch interferometric baseline coupled with an additional roll correction (~ 0.0075°), or equivalent phase correction (~ 0.0435 radians), provides an improved calibration of the interferometric SARIn mode.

We extend the potential use of SARIn data by showing the influence of surface conditions, especially melt, on the return waveforms, and that it is possible to detect and measure the height of summer supraglacial lakes in West Greenland. A supraglacial lake can provide a strong radar target in the waveform, stronger than the initial POCA return, if viewed at near normal incidence. This provides an ideal situation for swath processing and we demonstrate height accuracies of ~ 0.5 m for two lake sites, one in the accumulation zone and one in the ablation zone, which were measured every year from 2010 or 2011 to 2016. Each year the lake in the ablation zone was viewed in June by ascending passes and then 5.5 days later by descending passes which allows an approximate estimate of the filling rate. The results suggest that CryoSat waveform data and measurements of supraglacial lake height change could complement the use of optical satellite and be helpful as proxy indicators for surface melt around Greenland.


Citation: Gray, L., Burgess, D., Copland, L., Dunse, T., Langley, K., and Moholdt, G.: Improved processing and calibration of the interferometric mode of the CryoSat radar altimeter allows height measurements of supraglacial lakes in west Greenland, The Cryosphere Discuss., doi:10.5194/tc-2016-277, in review, 2016.
Laurence Gray et al.
Laurence Gray et al.
Laurence Gray et al.

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Short summary
We use surface height data from West Greenland and Devon Ice cap to check the performance of the new interferometric mode of the ESA CryoSat radar altimeter. The detailed height comparison allows an improved system calibration and processing methodology, and measurement of the height of supraglacial lakes which form each summer around the periphery of the Greenland Ice Cap. We believe that future satellite radar altimeters should employ this technology.
We use surface height data from West Greenland and Devon Ice cap to check the performance of the...
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