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Current PhD Research:
Meltwater flow through the Greenland Ice Sheet: To aid in the large scale characterization of the near-surface snow in the percolation facies, space-borne radar remote sensing is utilized. Due to the unique backscatter properties of the percolation facies, radar scatterometry can be used to detect melt features such as ice pipes, ice lenses and other impermeable boundaries. RADARSAT and past synthetic aperture radar (SAR) instruments provide high resolution images of the ice sheet surface. Dry snow will appear grey due to multiple scattering with the snowpack. Wet snow appears very dark due to spectral reflectance off the wet surface of the ice sheet. Finally, dry snow containing melt features will appear bright due to scattering off the dense lenses and pipes. Thus we can use radar to determine where and when melt occurs on the ice sheet and hopefully, how that meltwater travels through the snowpack. I am working on this project under the direction of Dr. Tad Pfeffer of INSTAAR, Dr. Konrad Steffen of CIRES at the University of Colorado and Dr. Waleed Abdalati of NASA Headquarters and the NASA Goddard Space Flight Center. Please visit Ursula Rick's homepage at INSTAAR |
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