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GEOPHYSICAL RESEARCH LETTERS,
VOL. 32,
L23S08,
5 PP., 2005
doi:10.1029/2005GL025070
ICESat's new perspective on ice shelf rifts: The vertical dimension
Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, La Jolla, California, USA
Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, La Jolla, California, USA
Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, La Jolla, California, USA
Department of Geophysical Sciences, University of Chicago, Chicago, Illinois, USA
The small footprint (∼70 m) and ∼172 m along-track spacing of the Geoscience Laser Altimeter System (GLAS) on the Ice, Cloud and land Elevation Satellite (ICESat) provides unprecedented horizontal resolution for a satellite altimeter. This enables ICESat to map many previously unresolved features on ice shelves, such as crevasses, rifts, grounding zones and ice fronts. We present examples of ICESat-derived elevation data showing topography over rifts on the Amery and Ross ice shelves, widths of rifts and as estimates of the thickness of mélange (a collection of ice and snow trapped inside the rifts). We show that mélange thickness remains constant over the ICESat data period and tends to be thicker in older rifts. We validate the ICESat-derived mélange depth estimate with an in situ measurement on the Ross Ice Shelf.
Received 28 October 2005; accepted 28 October 2005; published 1 December 2005.
Citation: (2005), ICESat's new perspective on ice shelf rifts: The vertical dimension, Geophys. Res. Lett., 32, L23S08, doi:10.1029/2005GL025070.
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