A comparison of basal reflectivity and ice velocity in East Antarctica
Ground-based radio echo sounding data acquired along the 1700 km US-ITASE traverse have been used to determine ice attenuation and relative basal reflectivity across the major catchments funneling ice from East Antarctica to the Ross Ice Shelf. We find that basal reflectivity varies locally by up to...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2010-10-01
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| Series: | The Cryosphere |
| Online Access: | http://www.the-cryosphere.net/4/447/2010/tc-4-447-2010.pdf |