Seabed topography beneath Larsen C Ice Shelf from seismic soundings

Seismic reflection soundings of ice thickness and seabed depth were acquired on the Larsen C Ice Shelf in order to test a sub-ice shelf bathymetry model derived from the inversion of IceBridge gravity data. A series of lines was collected, from the Churchill Peninsula in the north to the Joerg Penin...

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Bibliographic Details
Main Authors: A. M. Brisbourne, A. M. Smith, E. C. King, K. W. Nicholls, P. R. Holland, K. Makinson
Format: Article
Language:English
Published: Copernicus Publications 2014-01-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/8/1/2014/tc-8-1-2014.pdf