Grounding-line basal melt rates determined using radar-derived internal stratigraphy

We use ice-penetrating radar data across grounding lines of Siple Dome and Roosevelt Island, Antarctica, to measure the spatial pattern, magnitude and duration of sub-ice-shelf melting at these locations. Stratigraphic layers across the grounding line show, in places, a large-amplitude downwarp at,...

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Bibliographic Details
Main Authors: Catania, Ginny, Hulbe, Christina L., Conway, Howard
Format: Text
Language:unknown
Published: PDXScholar 2010
Subjects:
Online Access:https://pdxscholar.library.pdx.edu/geology_fac/22
https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1021&context=geology_fac