We used a coherent radar depth sounder operating at 150 MHz to collect
ice thickness data on outlet glaciers in northwestern Greenland. The
radar data were collected in conjunction with laser surface elevation
measurements and were tagged with GPS information for accurate geoloca
tion. The radar signals were corrupted by multiple echoes between the
aircraft and the ice surface, as well as between the ice surface and t
he ice-bedrock interface. We applied the homomorphic deconvolution tec
hnique to remove multiple echoes successfully and have identified the
grounding line of a long ice shelf in northwestern Greenland.