DocumentCode :
1266990
Title :
Validation of Airborne FMCW Radar Measurements of Snow Thickness Over Sea Ice in Antarctica
Author :
Galin, Natalia ; Worby, Anthony ; Markus, Thorsten ; Leuschen, Carl ; Gogineni, Prasad
Author_Institution :
Centre for Polar Obs. & Modelling, Univ. Coll. London, London, UK
Volume :
50
Issue :
1
fYear :
2012
Firstpage :
3
Lastpage :
12
Abstract :
Antarctic sea ice and its snow cover are integral components of the global climate system, yet many aspects of their vertical dimensions are poorly understood, making their representation in global climate models poor. Remote sensing is the key to monitoring the dynamic nature of sea ice and its snow cover. Reliable and accurate snow thickness data are currently a highly sought after data product. Remotely sensed snow thickness measurements can provide an indication of precipitation levels, predicted to increase with effects of climate change in the polar regions. Airborne techniques provide a means for regional-scale estimation of snow depth and distribution. Accurate regional-scale snow thickness data will also facilitate an increase in the accuracy of sea ice thickness retrieval from satellite altimeter freeboard estimates. The airborne data sets are easier to validate with in situ measurements and are better suited to validating satellite algorithms when compared with in situ techniques. This is primarily due to two factors: better chance of getting coincident in situ and airborne data sets and the tractability of comparison between an in situ data set and the airborne data set averaged over the footprint of the antennas. A 2-8-GHz frequency modulated continuous wave (FMCW) radar loaned by the Center for Remote Sensing of Ice Sheets to the Australian Antarctic Division is used to measure snow thickness over sea ice in East Antarctica. Provided with the radar design parameters, the expected performance parameters of the radar are summarized. The necessary conditions for unambiguous identification of the air/snow and snow/ice layers for the radar are presented. Roughnesses of the snow and ice surfaces are found to be dominant determinants in the effectiveness of layer identification for this radar. Finally, this paper presents the first in situ validated snow thickness estimates over sea ice in Antarctica derived from an FMCW radar on a helicopterborne platform.
Keywords :
geophysical techniques; remote sensing by radar; sea ice; snow; Antarctica; Australian Antarctic Division; Center for Remote Sensing of Ice Sheets; FMCW radar; air-snow layer; airborne FMCW radar measurements; airborne techniques; frequency modulated continuous wave; global climate models; global climate system; helicopterborne platform; ice surfaces; polar regions; precipitation levels; radar design parameters; regional-scale estimation; satellite algorithms; satellite altimeter freeboard estimates; sea ice; snow cover; snow thickness data; snow-ice layer; Antarctica; Laser radar; Sea ice; Snow; Spaceborne radar; Airborne; Antarctica; frequency modulated continuous wave (FMCW); sea ice; snow;
fLanguage :
English
Journal_Title :
Geoscience and Remote Sensing, IEEE Transactions on
Publisher :
ieee
ISSN :
0196-2892
Type :
jour
DOI :
10.1109/TGRS.2011.2159121
Filename :
5944968
Link To Document :
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