Computer Science – Sound
Scientific paper
Jun 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001georl..28.2241f&link_type=abstract
Geophysical Research Letters, Volume 28, Issue 11, p. 2241-2244
Computer Science
Sound
20
Global Change: Remote Sensing, Hydrology: Glaciology, Hydrology: Snow And Ice, Oceanography: General: Arctic And Antarctic Oceanography
Scientific paper
We present a map of the marine ice accreted to the base of the Amery Ice Shelf (AIS), East Antarctica. This map is obtained by converting a Digital Elevation Model (DEM) of the AIS generated from satellite radar altimeter data to an ice thickness map, assuming hydrostatic equilibrium, and subtracting from that a second ice thickness map, derived from airborne radio-echo sounding (RES) measurements. The RES signal does not penetrate the marine ice, so the measurement is only to the meteoric-marine ice boundary, and therefore the difference between the two maps is the marine ice thickness. The marine ice is up to 190 m thick and accounts for about 9% of the shelf volume. It is concentrated in the northwest of the shelf, a result of the clockwise ocean circulation in the cavity below.
Allison Ian
Fricker Helen Amanda
Popov Sergey
Young Neal
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